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1

Vos, Charles J. "Pumped Storage Plants in Lowland Regions." Structural Engineering International 4, no. 2 (May 1994): 99–100. http://dx.doi.org/10.2749/101686694780650904.

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2

Ogawa, Toyokazu, Takumi Shidahara, Shigetaka Nakanishi, Takashi Yamamoto, Kazuyuki Yoneyama, Tadahiko Okumura, and Tsutomu Hashimoto. "Storage Capacity Assessment in Japan: Comparative Evaluation of CO2 aquifer storage capacities across regions." Energy Procedia 1, no. 1 (February 2009): 2685–92. http://dx.doi.org/10.1016/j.egypro.2009.02.037.

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3

Crotogino, Fritz, Gregor-Sönke Schneider, and David J. Evans. "Renewable energy storage in geological formations." Proceedings of the Institution of Mechanical Engineers, Part A: Journal of Power and Energy 232, no. 1 (September 13, 2017): 100–114. http://dx.doi.org/10.1177/0957650917731181.

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With the transition to renewable energies and, above all, strongly fluctuating electricity from wind and solar energy, there will be a need for energy storage in the future. For central grid-scale storages, underground geological storage, similar to those already used for fossil fuels, is in the first place under review. Compressed Air Energy Storages have already been successfully used to provide minutes to hours reserve. For storage capacities in the day to week range, storage is required on a chemical rather than a mechanical basis, through either the conversion of electricity into pure hydrogen (H2) or the generation of mixtures of natural gas and synthetic methane. The latter – the so-called power-to-gas option – allows the use of the existing gas infrastructure. A likely first choice for the storage of H2 or H2-SNG mixtures are man-made salt caverns. The suitability of porous rock storage (depleted hydrocarbon reservoirs or water-bearing reservoirs – aquifers) is still under investigation. Interest in porous rock storage options arises, inter alia, from the fact that many regions of Europe lack suitable salt deposits. Favorable salt deposits exist in the UK, notably in the Cheshire Basin to the west and in eastern England, with six salt cavern-hosted facilities operated as natural gas storages. In any case, underground gas storages are characterized by high safety and low environmental impact.
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4

Chen, Zheng, Wenjie Wang, Weiguo Jiang, Mingliang Gao, Beibei Zhao, and Yunwei Chen. "The Different Spatial and Temporal Variability of Terrestrial Water Storage in Major Grain-Producing Regions of China." Water 13, no. 8 (April 9, 2021): 1027. http://dx.doi.org/10.3390/w13081027.

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Irrigation is an important factor affecting the change of terrestrial water storage (TWS), especially in grain-producing areas. The Northeast China Plain (NECP), the Huang-Huai-Hai Plain (HHH) and the middle and lower reaches of the Yangtze River Basin Plain (YRB) are major grain-producing regions of China, with particular climate conditions, crops and irrigation schemes. However, there are few papers focusing on the different variation pattern of water storage between NECP, HHH and YRB. In this paper, the characteristics of terrestrial water storage anomaly (TWSA) and groundwater storage in the three regions mentioned above from 2003 to 2014 were analyzed, and the main reasons for water storage variations in the three regions were also discussed. The result shows that although effective irrigated areas increased in all three regions, TWSA only decreased in HHH and TWSA in the other two regions have shown an increasing trend. Spatially, the water storage deficit was more serious in middle and south NECP and HHH. In the three regions, water storage variations were impacted by meteorological condition and anthropogenic stress (e.g., irrigation). However, irrigation water consumption has a greater impact on water storage deficit in HHH than the other two regions, and water storage variation in YRB was mainly impacted by meteorological conditions. In this case, we suggest that the structure of agricultural planting in HHH should be adjusted to reduce the water consumption for irrigation.
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5

Pansino, Stephen, and Benoit Taisne. "How Magmatic Storage Regions Attract and Repel Propagating Dikes." Journal of Geophysical Research: Solid Earth 124, no. 1 (January 2019): 274–90. http://dx.doi.org/10.1029/2018jb016311.

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6

Frühwald, A. "Technological Properties of Wood from Trees in Polluted Regions." IAWA Journal 7, no. 4 (1986): 389–97. http://dx.doi.org/10.1163/22941932-90001009.

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Wood quality from about 230 healthy and diseased fir, spruce, pine and beech trees from various locations in West Germany was tested. In general results are satisfactory for mechanical wood properties, but some physical, chemical and biological indicators lead to the conclusion that logs from heavily diseased trees may be attacked a !ittle earlier and faster by microorganisms during storage. Width of growth rings is reduced in severely damaged softwood trees on most locations whereas beech shows no significant reduction. Declining health of the trees had no or little influence on wood density; the modulus of elasticity and strength were at normal levels and independent of tree damage. Width and moisture content of sapwood were reduced little in pines but more in spruce and fir. A tendency to a more intensely developed irregular brown heartwood in severeIy damaged beech trees could not be proved until now. Storage of spruce in a log yard for four months has shown a slightly faster development of discoloration caused by fungi in diseased trees whereas after seven months wood from healthy trees was more discoloured. After storage strength properties are not or only slightly reduced, but no difference was found between trees assigned to the various health classes. After two years of storage under sprinkling water, pine logs from healthy and diseased trees show no difference in discoloration.
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7

Hamadina, Elsie. "Dry matter, Free Sugar and Starch Changes in Tuber Regions of White Yam (Dioscorea rotundata Poir.), and the Effect of Storage Environment." JOURNAL OF ADVANCES IN AGRICULTURE 4, no. 1 (April 8, 2015): 303–9. http://dx.doi.org/10.24297/jaa.v4i1.4298.

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This study was conducted to determine the changes in dry matter (DM), free sugar (FS) and starch contents in the three yam (D. rotundata) tuber regions under two storage environmental conditions (natural light- yam barn, or and darkness). Three varieties of D. rotundata (alaako, Dodoro and Odo) were studied. The dry matter content of the Head region was the highest (28.6%), followed by the Middle (26.9%) and Tail (22.3%) regions. Change in dry matter content of the tuber is mainly due to rapid changes in the dry matter content of the Tail region over time. Storage environment significantly (P< 0.05) affected dry matter content of the three tuber regions at 8 and 16 weeks in storage (WIS). Head regions per variety were lower in dry matter when stored under Light than in the Dark at 8 WIS, while the reverse was the case for the Tail. This may relate to the release of endodormancy. By 16 WIS, when tubers stored under Light had well developed sprouts and those stored in the Dark only showed the first sign of sprouting, all Head regions had higher dry matter content under Light than in Dark storage. This may be due to the presence of sprouts. Storage environment did not significantly affect starch content at the various tuber regions. Head regions had higher percentage free sugar content under Light than Dark storage, and these effects were manifested between 8 and 16 WIS.
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8

de Boer-Euser, Tanja, Leo-Juhani Meriö, and Hannu Marttila. "Understanding variability in root zone storage capacity in boreal regions." Hydrology and Earth System Sciences 23, no. 1 (January 10, 2019): 125–38. http://dx.doi.org/10.5194/hess-23-125-2019.

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Abstract. The root zone storage capacity (Sr) of vegetation is an important parameter in the hydrological behaviour of a catchment. Traditionally, Sr is derived from soil and vegetation data. However, more recently a new method has been developed that uses climate data to estimate Sr based on the assumption that vegetation adapts its root zone storage capacity to overcome dry periods. This method also enables one to take into account temporal variability of derived Sr values resulting from changes in climate or land cover. The current study applies this new method in 64 catchments in Finland to investigate the reasons for variability in Sr in boreal regions. Relations were assessed between climate-derived Sr values and climate variables (precipitation-potential evaporation rate, mean annual temperature, max snow water equivalent, snow-off date), detailed vegetation characteristics (leaf cover, tree length, root biomass), and vegetation types. The results show that in particular the phase difference between snow-off date and onset of potential evaporation has a large influence on the derived Sr values. Further to this it is found that (non-)coincidence of snow melt and potential evaporation could cause a division between catchments with a high and a low Sr value. It is concluded that the climate-derived root zone storage capacity leads to plausible Sr values in boreal areas and that, apart from climate variables, catchment vegetation characteristics can also be directly linked to the derived Sr values. As the climate-derived Sr enables incorporating climatic and vegetation conditions in a hydrological parameter, it could be beneficial to assess the effects of changing climate and environmental conditions in boreal regions.
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9

Dupraz, Elsa, Aline Roumy, Thomas Maugey, and Michel Kieffer. "Rate-storage regions for Extractable Source Coding with side information." Physical Communication 37 (December 2019): 100845. http://dx.doi.org/10.1016/j.phycom.2019.100845.

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10

Shogenova, Alla, Kazbulat Shogenov, Rein Vaher, Jüri Ivask, Saulius Sliaupa, Thomas Vangkilde-Pedersen, Mai Uibu, and Rein Kuusik. "CO2 geological storage capacity analysis in Estonia and neighbouring regions." Energy Procedia 4 (2011): 2785–92. http://dx.doi.org/10.1016/j.egypro.2011.02.182.

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11

Niegemann, Jens, Richard Diehl, and Kurt Busch. "Efficient low-storage Runge–Kutta schemes with optimized stability regions." Journal of Computational Physics 231, no. 2 (January 2012): 364–72. http://dx.doi.org/10.1016/j.jcp.2011.09.003.

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12

Lauenroth, W. K., D. R. Schlaepfer, and J. B. Bradford. "Ecohydrology of Dry Regions: Storage versus Pulse Soil Water Dynamics." Ecosystems 17, no. 8 (October 1, 2014): 1469–79. http://dx.doi.org/10.1007/s10021-014-9808-y.

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13

Liu, Qing, Dongdong Yang, Lei Cao, and Bruce Anderson. "Assessment and Prediction of Carbon Storage Based on Land Use/Land Cover Dynamics in the Tropics: A Case Study of Hainan Island, China." Land 11, no. 2 (February 6, 2022): 244. http://dx.doi.org/10.3390/land11020244.

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Land use and land cover (LULC) change in tropical regions can cause huge amounts of carbon loss and storage, thus significantly affecting the global climate. Due to the differences in natural and social conditions between regions, it is necessary to explore the correlation mechanism between LULC and carbon storage changes in tropical regions from a broader geographical perspective. This paper takes Hainan Island as the research object, through the integration of the CA-Markov and Integrated Valuation of Ecosystem Services and Tradeoffs (InVEST) models, based on multi-source data, analyses the dynamics of LULC and carbon storage from 1992 to 2019 and the relationship between the two, and predicts future LULC and carbon storage under different scenarios. The results show that (1) the built-up land area of Hainan Island expanded from 103.59 km2 to 574.83 km2 from 1992 to 2019, an increase of 454.91%; the area of cropland and shrubland decreased; and the area of forest increased. (2) Carbon storage showed an upward trend during 1992–2000, and a downward trend during 2000–2019. Overall, LULC changes during 1992–2019 reduced carbon storage by about 1.50 Tg. (3) The encroachment of cropland in built-up land areas is the main reason for the reduction of carbon storage. The conversion of shrubland to forest is the main driving force for increasing carbon storage. The increase and decrease of carbon storage have obvious spatial clustering characteristics. (4) In the simulation prediction, the natural trend scenario (NT), built-up land priority scenario (BP) and ecological priority scenario (EP) reduce the carbon storage of Hainan Island, and the rate of decrease is BP> NT > EP. The cropland priority scenario (CP) can increase the LULC carbon storage, and the maximum increase in 2050 can reach 0.79 Tg. This paper supplements and improves the understanding of the correlation between LULC and carbon storage changes in tropical regions, and can provide guidance for the optimization of LULC structure in tropical regions with high economic development from a low-carbon perspective.
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14

Li, Ning, Zhi-Qiang Liu, Guo-Dong Niu, Jian Zhang, Jun-Ping Li, and Fan Zhang. "Numerical simulation considering the effect of uneven frost heave on tunnel structure in cold regions." Thermal Science 25, no. 6 Part B (2021): 4545–52. http://dx.doi.org/10.2298/tsci2106545l.

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Freezing damage is one of the main diseases of tunnels in cold regions. Water storage behind the lining is a necessary condition for freezing damage. Compared with the previous condition of uniform water storage behind the lining, this paper explores the influence of water storage and frost heave at different positions on tunnel structure in cold regions. Based on the theory of thermo-hydro-mechan?ical coupling. The finite element model of tunnel surrounding rock in cold area under different positions and different water content is established and compared by using COMSOL software, the mechanical characteristics of tunnel lining under different water storage positions behind the lining are studied, and the influence of frost heave at different positions on tunnel structure is explored. The numerical simulation results show that no matter where the local water storage area is lo?cated, the area with the largest frost heave force is located in the lining structure, close to the surrounding rock. Different local water storage positions will also have different influences on the tunnel structure. In the same water storage area, the frost heave force will increase with the decrease of temperature.
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15

Zhang, C., Y. Peng, J. Chu, C. A. Shoemaker, and A. Zhang. "Integrated hydrological modelling of small- and medium-sized water storages with application to the upper Fengman Reservoir Basin of China." Hydrology and Earth System Sciences 16, no. 11 (November 6, 2012): 4033–47. http://dx.doi.org/10.5194/hess-16-4033-2012.

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Abstract. Hydrological simulation in regions with a large number of water storages is difficult due to inaccurate water storage data. To address this issue, this paper presents an improved version of SWAT2005 (Soil and Water Assessment Tool, version 2005) using Landsat, a satellite-based dataset, an empirical storage classification method and some empirical relationships to estimate water storage and release from the various sizes of flow detention and regulation facilities. The SWAT2005 is enhanced by three features: (1) a realistic representation of the relationships between the surface area and volume of each type of water storages, ranging from small-sized flow detention ponds to medium- and large-sized reservoirs with the various flow regulation functions; (2) water balance and transport through a network combining both sequential and parallel streams and storage links; and (3) calibrations for both physical and human interference parameters. Through a real-world watershed case study, it is found that the improved SWAT2005 more accurately models small- and medium-sized storages than the original model in reproducing streamflows in the watershed. The improved SWAT2005 can be an effective tool to assess the impact of water storage on hydrologic processes, which has not been well addressed in the current modelling exercises.
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16

Velpuri, Naga Manohar, Gabriel B. Senay, Jessica M. Driscoll, Samuel Saxe, Lauren Hay, William Farmer, and Julie Kiang. "Gravity Recovery and Climate Experiment (GRACE) Storage Change Characteristics (2003–2016) over Major Surface Basins and Principal Aquifers in the Conterminous United States." Remote Sensing 11, no. 8 (April 18, 2019): 936. http://dx.doi.org/10.3390/rs11080936.

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In this research, we characterized the changes in the Gravity Recovery and Climate Experiment (GRACE) monthly total water storage anomaly (TWSA) in 18 surface basins and 12 principal aquifers in the conterminous United States during 2003–2016. Regions with high variability in storage were identified. Ten basins and four aquifers showed significant changes in storage. Eight surface basins and eight aquifers were found to show decadal stability in storage. A pixel-based analysis of storage showed that the New England basin and North Atlantic Coastal Plain aquifer showed the largest area under positive storage change. By contrast, the Lower Colorado and California basins showed the largest area under negative change. This study found that historically wetter regions (with more storage) are becoming wetter, and drier regions (with less storage) are becoming drier. Fourier analysis of the GRACE data showed that while all basins exhibited prominent annual periodicities, significant sub-annual and multi-annual cycles also exist in some basins. The storage turnover period was estimated to range between 6 and 12 months. The primary explanatory variable (PEV) of TWSA was identified for each region. This study provides new insights on several aspects of basin or aquifer storage that are important for understanding basin and aquifer hydrology.
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17

Longuevergne, L., C. R. Wilson, B. R. Scanlon, and J. F. Crétaux. "GRACE water storage estimates for the Middle East and other regions with significant reservoir and lake storage." Hydrology and Earth System Sciences 17, no. 12 (December 5, 2013): 4817–30. http://dx.doi.org/10.5194/hess-17-4817-2013.

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Abstract. While GRACE (Gravity Recovery and Climate Experiment) satellites are increasingly being used to monitor total water storage (TWS) changes globally, the impact of spatial distribution of water storage within a basin is generally ignored but may be substantial. In many basins, water is often stored in reservoirs or lakes, flooded areas, small aquifer systems, and other localized regions with areas typically below GRACE resolution (~200 000 km2). The objective of this study was to assess the impact of nonuniform water storage distribution on GRACE estimates of TWS changes as basin-wide averages, focusing on surface water reservoirs and using a priori information on reservoir storage from radar altimetry. Analysis included numerical experiments testing effects of location and areal extent of the localized mass (reservoirs) within a basin on basin-wide average water storage changes, and application to the lower Nile (Lake Nasser) and Tigris–Euphrates basins as examples. Numerical experiments show that by assuming uniform mass distribution, GRACE estimates may under- or overestimate basin-wide average water storage by up to a factor of ~2, depending on reservoir location and areal extent. Although reservoirs generally cover less than 1% of the basin area, and their spatial extent may be unresolved by GRACE, reservoir storage may dominate water storage changes in some basins. For example, reservoir storage accounts for ~95% of seasonal water storage changes in the lower Nile and 10% in the Tigris–Euphrates. Because reservoirs are used to mitigate droughts and buffer against climate extremes, their influence on interannual timescales can be large. For example, TWS decline during the 2007–2009 drought in the Tigris–Euphrates basin measured by GRACE was ~93 km3. Actual reservoir storage from satellite altimetry was limited to 27 km3, but their apparent impact on GRACE reached 45 km3, i.e., 50% of GRACE trend. Therefore, the actual impact of reservoirs would have been greatly underestimated (27 km3) if reservoir storage changes were assumed uniform in the basin. Consequently, estimated groundwater contribution from GRACE would have been largely overestimated in this region if the actual distribution of water was not explicitly taken into account. Effects of point masses on GRACE estimates are not easily accounted for via simple multiplicative scaling, but in many cases independent information may be available to improve estimates. Accurate estimation of the reservoir contribution is critical, especially when separating estimating groundwater storage changes from GRACE total water storage (TWS) changes. Because the influence of spatially concentrated water storage – and more generally water distribution – is significant, GRACE estimates will be improved by combining independent water mass spatial distribution information with GRACE observations, even when reservoir storage is not the dominant mechanism. In this regard, data from the upcoming Surface Water Ocean Topography (SWOT) satellite mission should be an especially important companion to GRACE-FO (Follow-On) observations.
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18

Brand, Martha Andreia, Graciela Inês Bolzon de Muñiz, Waldir Ferreira Quirino, and José Otávio Brito. "Influence of storage time on the quality of biomass for energy production in humid subtropical regions." CERNE 16, no. 4 (December 2010): 531–37. http://dx.doi.org/10.1590/s0104-77602010000400012.

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This work aims to determine an optimal storage time of forest biomass for use in energy production, through analysis of variations in physical and chemical properties of with bark timber over the storage period. The study was conducted in the municipality of Lages, SC, over a span of 18 months. The experiment used with bark logs of Pinus taeda and Eucalyptus dunnii, with varying diameters, and slabs of Pinus spp., stored in piles. The material was sampled freshly harvested (control), after two, after four and after six months of storage. Four lots were used, harvested and stored at the spring, summer, autumn and winter seasons. Properties being assessed included moisture content (wet basis), gross calorific value, net calorific value and ash content. Results demonstrated that storage time influenced moisture content and net calorific value, yet it had no influence on gross calorific value and ash content. Optimal storage time ranged from two to four months, depending on the species, form of biomass and storage season. The best behavior regarding quality after storage was from Pinus slabs, followed by Eucalyptus logs and Pinus logs, the latter showing the worst behavior.
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19

Guo, Xiaomin, Xiaowei Chuai, and Xianjin Huang. "A Land Use/Land Cover Based Green Development Study for Different Functional Regions in the Jiangsu Province, China." International Journal of Environmental Research and Public Health 16, no. 7 (April 10, 2019): 1277. http://dx.doi.org/10.3390/ijerph16071277.

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Land use/land cover (LULC) change can strongly affect carbon storage in terrestrial ecosystems. The rapid development of China’s economy has formed different functional regions. These functional regions profoundly affect land use patterns. Thus, assessing the carbon storage induced by LULC changes is significant for green development. Selecting the typical region of the Jiangsu Province as the study area, this study first examines the research associated with the regional functional characteristics and various high accuracy data and methods have been used to greatly improve the research accuracy. The results showed that from 1995 to 2015, approximately 10.26% of the entire land area had LULC type changes. Additionally, decreases in the built-up land expansion and ecological land were the main LULC change characteristics, which are mainly affected by socioeconomic development. The total carbon storage of the Jiangsu Province decreased by 714.03 × 104 t and the four regions all presented decreasing carbon storage levels. The economically developed regions presented a more obvious loss of carbon. The region with small LULC changes had a lower carbon loss. The land transfer of cultivated land to built-up land is the main transfer type causing the carbon storage loss. This study investigates the human-environmental interactions from the new perspective of functional zoning and, thus, it enriches the comparative analysis of carbon storage in functional regions and provides references for the green development of a developing country’s developed areas.
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20

Xu, Zhicheng, Jun Liu, and Zhuonan Li. "The adaptive assessment method for different energy storage applications in large-scale re-electrical load access regions." E3S Web of Conferences 165 (2020): 06030. http://dx.doi.org/10.1051/e3sconf/202016506030.

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In the context of energy transformation, re-electrification has become an important way to build a clean and low-carbon energy system. The large-scale re-electrical load access further increases the flexibility requirements on the user demand side. The application of the energy storage system (ESS) can not only improve the degree of electrification of the energy system but also improve the energy utilization efficiency. This paper analyzes the different development modes and key characteristics of energy storage on the power supply side, grid side and demand side in large-scale re-electrical load access areas. Five dimensions (such as storage security, technology maturity, system cost, storage scenario suitability and storage scalability) are selected to characterize the feasibility of a certain energy storage technology in a given application scenario. For different application scenarios, studying the appropriate development mode and its adaptability to the environment will help the healthy and sustainable development of energy storage.
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21

Longuevergne, L., C. R. Wilson, B. R. Scanlon, and J. F. Crétaux. "GRACE water storage estimates for the Middle East and other regions with significant reservoir and lake storage." Hydrology and Earth System Sciences Discussions 9, no. 10 (October 1, 2012): 11131–59. http://dx.doi.org/10.5194/hessd-9-11131-2012.

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Abstract. While GRACE (Gravity Recovery and Climate Experiment) satellites are increasingly being used to monitor water storage changes globally, the impact of spatial distribution of water storage within a basin is generally ignored but may be substantial. In many basins, water may be stored in reservoirs, lakes, flooded areas, small aquifer systems, and other localized regions with sizes typically below GRACE resolution. The objective of this study was to assess the impact of non-uniform water storage distribution on GRACE estimates as basin-wide averages, focusing on surface water reservoirs. Analysis included numerical experiments testing the effect of mass size and position within a basin, and application to the Lower Nile (Lake Nasser) and Tigri–Euphrates (TE) basins as examples. Numerical experiments show that by assuming uniform mass distribution, GRACE estimates may under- or over-estimate basin-average water storage by up to a factor of two, depending on reservoir location and extent. Although their spatial extent may be unresolved by GRACE, reservoir storage may dominate in some basins. For example, it accounts for 95% of seasonal variations in the Lower Nile and 10% in the TE basins. Because reservoirs are used to mitigate droughts and buffer against climate extremes, their influence on interannual time scales can be large, for example accounting for 50% of total water storage decline during the 2007–2009 drought in the TE basin. Effects on GRACE estimates are not easily accounted for via simple multiplicative scaling, but in many cases independent information may be available to improve estimates. Accurate estimation of the reservoir contribution is critical, especially when separating groundwater from GRACE total water storage changes. Because the influence of spatially concentrated water storage – and more generally water distribution – is significant, GRACE estimates will be improved when it is possible to combine independent spatial distribution information with GRACE observations, even when reservoir storage is not a major factor. In this regard, data from the upcoming Surface Water Ocean Topography (SWOT) satellite mission should be an especially important companion to GRACE-FO observations.
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22

Chu, C. L. "Effects of Storage Temperature, Storage Atmosphere, and Growing Region on Internal Browning Disorder of `McIntosh' Apples." HortTechnology 9, no. 1 (January 1999): 75–78. http://dx.doi.org/10.21273/horttech.9.1.75.

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Our study found that storage temperature, storage atmosphere and growing region interactively affect the probability of internal browning disorder in `McIntosh' apples (Malus domestica Borkh.). Higher incidence of internal browning occurred in apples stored for 6 months at 1 °C (34 °F) in controlled atmosphere (CA) with 2.5% O2 + 1.5% CO2 or in CA with 1.0% O2 + 0.5% CO2 than apples stored at 1 °C in air or stored at 3 °C (37 °F) in air or CA conditions. The magnitude of the incidence of internal browning varied among apples harvested from different growing regions. Apples from London, Ontario, Canada were less tolerant to these two storage conditions and therefore greater number of fruit developed internal browning than apples from other regions. In addition, apples from the London growing region and stored at 1 °C in CA with 1.0% O2 + 0.5% CO2 had greater probability of internal browning than apples stored at 1 °C in CA with 2.5% O2 + 1.5% CO2. However, there was no difference between these two CA storage conditions in causing internal browning among apples harvested from other three growing regions. Few apples showed internal browning when they were stored at 3 °C, no matter of what storage atmosphere was used. Therefore, internal browning disorder can be avoided or significantly reduced by storing apples at 3 instead of 1 °C, in these two CA conditions. Internal browning disorder will not be a risk if apples are stored in air at 1 or 3 °C.
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23

Shi, Pengfei, Tao Yang, Chong-Yu Xu, Bin Yong, Ching-Sheng Huang, Zhenya Li, Youwei Qin, Xiaoyan Wang, Xudong Zhou, and Shu Li. "Rainfall–Runoff Processes and Modelling in Regions Characterized by Deficiency in Soil Water Storage." Water 11, no. 9 (September 6, 2019): 1858. http://dx.doi.org/10.3390/w11091858.

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The partial runoff is complicated in semi-arid and some semi-humid zones in terms of what the runoff generates in partial vertical positions. The partial runoff is highlighted by horizontal soil heterogeneity as well. How to identify the partial runoff and develop a variable threshold for runoff generation is a great difficulty and challenge. In this work, the partial runoff is identified by using a variable active runoff layer structure, and a variable soil water storage capacity is proposed to act as a threshold for runoff generation. A variable layer-based runoff model (VLRM) for simulating the complex partial runoff was therefore developed, using dual distribution curves for variable soil water storage capacity over basin. The VLRM is distinct in that the threshold for runoff generation is denoted by variable soil water storage capacity instead of infiltration capacity or constant soil water storage capacity. A series of flood events in two typical basins of North China are simulated by the model, and also by the Xinanjiang model. Results demonstrate that the new threshold performs well and the new model outperforms the Xinanjiang model. The approach improves current hydrological modelling for complex runoff in regions with large deficiencies in soil water storage.
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24

Haberichter, Sandra L., Paula Jacobi, and Robert R. Montgomery. "Critical independent regions in the VWF propeptide and mature VWF that enable normal VWF storage." Blood 101, no. 4 (February 15, 2003): 1384–91. http://dx.doi.org/10.1182/blood-2002-07-2281.

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Von Willebrand factor (VWF) is synthesized in endothelial cells, where it is stored in Weibel-Palade bodies. Administration of 1-desamino-8-D-arginine-vasopressin (DDAVP) to patients with type 1 von Willebrand disease and to healthy individuals causes a rapid increase in plasma VWF levels. This increase is the result of stimulated release of VWF from Weibel-Palade bodies in certain beds of endothelial cells. The VWF propeptide (VWFpp) targets VWF to storage granules through a noncovalent association. The nature of the VWFpp/VWF interaction was investigated by using cross-species differences in VWF storage. While canine VWFpp traffics to storage granules and facilitates the multimerization of human VWF, it does not direct human VWF to storage granules. Since storage takes place after furin cleavage, this defect appears to be due to the defective interaction of canine VWFpp and human VWF. To determine the regions within VWFpp and VWF important for this VWFpp/VWF association and costorage, a series of human-canine chimeric VWFpp and propeptide-deleted VWF (Δpro) constructs were produced and expressed in AtT-20 cells. The intracellular localization of coexpressed proteins was examined by confocal microscopy. Two amino acids, 416 in VWFpp and 869 in the mature VWF molecule, were identified as being critical for the association and granular storage of VWF.
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Fragos, T., E. Rantsiou, and L. Vlahos. "On the distribution of magnetic energy storage in solar active regions." Astronomy & Astrophysics 420, no. 2 (May 28, 2004): 719–28. http://dx.doi.org/10.1051/0004-6361:20034570.

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Wang, Hua-Ning, Yan-Mei Cui, and Han He. "A logistic model for magnetic energy storage in solar active regions." Research in Astronomy and Astrophysics 9, no. 6 (May 27, 2009): 687–93. http://dx.doi.org/10.1088/1674-4527/9/6/007.

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Zhu, Xinrong, Hongyan Liu, Wenqi He, Lu Wu, and Feng Liu. "Regolith water storage patterns determine vegetation productivity in global karst regions." Geoderma 430 (February 2023): 116292. http://dx.doi.org/10.1016/j.geoderma.2022.116292.

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Barkouti, Amal, Mohamed Najib Melki, Abdullah Beyaz, and Slaheddine Khlifi. "Prediction of Wheat Storage Process Under Climate Change: A Case Study of Northwestern Regions of Tunisia." American Journal of Agricultural Science, Engineering, and Technology 7, no. 1 (December 29, 2022): 1–6. http://dx.doi.org/10.54536/ajaset.v7i1.1056.

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In this work, a simulation of the climate change impact on the wheat grain storage process in Northwestern regions of Tunisia was investigated based on grain aeration systems. This simulation was conducted by implementing the software package called Zephyrus for a period from 2041 to 2070 during storage season from the 01st of July to the 30th of November. The model estimates grain moisture content, grain temperature, and dry matter loss. The results showed a significant potential of the Zypherus strategy to maintain the grain moisture content around 12.2± 0.2% w.b. and to reduce grain temperatures from 35°C to 24 ± 1.5°C inside the silo. Consequently, under these values, the wheat storage process is considered safe and preserves wheat quality during the simulated storage period. Moreover, the wheat dry loss matter was about 0.8% during the whole storage period for each simulated year (approximately 0.15% per month).
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Greenwood, John S., and J. Derek Bewley. "Seed development in Ricinus communis cv. Hale (castor bean). III. Pattern of storage protein and phytin accumulation in the endosperm." Canadian Journal of Botany 63, no. 12 (December 1, 1985): 2121–28. http://dx.doi.org/10.1139/b85-299.

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The development of the endosperm of castor bean seed from its initial free nuclear state through to the end of maturation is presented. An investigation of the pattern of reserve accumulation in the endosperm at the light microscopy level revealed that the accumulation of soluble and insoluble storage proteins, and of phytin, does not occur simultaneously in all cells of the developing storage organ. Rates of reserve accumulation also vary among regions of the endosperm. Storage protein and phytin accumulation are initiated in a region midway between the periphery and central lumen of the endosperm by the early cotyledon stage of seed development. Afterwards, reserve deposition occurs more intensely in the proximal and more peripheral regions than in the distal and internal regions. A wave of reserve accumulation, or protein body maturation, proceeds from the more peripheral and the proximal regions to the more internal and distal regions as development continues. The last cells to complete reserve deposition are those in regions lying close to the endosperm lumen (into which the cotyledons have expanded) and the outermost two cell layers of the endosperm.
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Zhang, C., Y. Peng, J. Chu, and C. A. Shoemaker. "Integrated hydrological modelling of small- and medium-sized water storages with application to the upper Fengman Reservoir Basin of China." Hydrology and Earth System Sciences Discussions 9, no. 3 (March 28, 2012): 4001–43. http://dx.doi.org/10.5194/hessd-9-4001-2012.

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Abstract. Hydrological simulation in regions with a large number of water storages is difficult due to the inaccurate water storage data, including both topologic parameters and operational rules. To address this issue, this paper presents an improved version of SWAT2005 (Soil and Water Assessment Tool, version 2005) using the satellite-based dataset Landsat, an empirical storage classification method, and some empirical relationships to estimate water storage and release from the various levels of flow regulation facilities. The improved SWAT2005 is characterised by three features: (1) a realistic representation of the relationships between the water surface area and volume of each type of water storage, ranging from small-sized ponds for water flow regulation to large-sized and medium-sized reservoirs for water supply and hydropower generation; (2) water balance and transport through a network combining both sequential and parallel streams and storage links; and (3) calibrations for the physical parameters and the human interference parameters. Both the original and improved SWAT2005 are applied to the upper Fengman Reservoir Basin, and the results of these applications are compared. The improved SWAT2005 accurately models small- and medium-sized storages, indicating a significantly improved performance from that of the original model in reproducing streamflows.
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Chinnasamy, Pennan, and Revathi Ganapathy. "Long-term variations in water storage in Peninsular Malaysia." Journal of Hydroinformatics 20, no. 5 (November 7, 2017): 1180–90. http://dx.doi.org/10.2166/hydro.2017.043.

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Abstract Information on ongoing climate change impacts on water availability is limited for Asian regions, particularly for Peninsular Malaysia. Annual flash floods are common during peak monsoon seasons, while the dry seasons are hit by droughts, leading to socio-economic stress. This study, for the first time, analyzed the long-term trends (14 years, from 2002 to 2014) in terrestrial water storage and groundwater storage for Peninsular Malaysia, using Gravity Recovery And Climate Experiment data. Results indicate a decline in net terrestrial and groundwater storage over the last decade. Spatially, the northern regions are more affected by droughts, while the southern regions have more flash floods. Groundwater storage trends show strong correlations to the monsoon seasons, indicating that most of the shallow aquifer groundwater is used. Results also indicate that, with proper planning and management, excess monsoon/flash flood water can be stored in water storage structures up to the order of 87 billion liters per year. This can help in dry season water distribution and water transfer projects. Findings from this study can expand the understanding of ongoing climate change impacts on groundwater storage and terrestrial water storage, and can lead to better management of water resources in Peninsular Malaysia.
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Mu, C., T. Zhang, Q. Wu, X. Peng, B. Cao, X. Zhang, B. Cao, and G. Cheng. "Editorial: Organic carbon pools in permafrost regions on the Qinghai–Xizang (Tibetan) Plateau." Cryosphere 9, no. 2 (March 6, 2015): 479–86. http://dx.doi.org/10.5194/tc-9-479-2015.

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Abstract. The current Northern Circumpolar Soil Carbon Database did not include organic carbon storage in permafrost regions on the Qinghai–Xizang (Tibetan) Plateau (QXP). In this study, we reported a new estimation of soil organic carbon (SOC) pools in the permafrost regions on the QXP up to 25 m depth using a total of 190 soil profiles. The SOC pools were estimated to be 17.3 ± 5.3 Pg for the 0–1 m depth, 10.6 ± 2.7 Pg for the 1–2 m depth, 5.1 ± 1.4 Pg for the 2–3 m depth and 127.2 ± 37.3 Pg for the layer of 3–25 m depth. The percentage of SOC storage in deep layers (3–25 m) on the QXP (80%) was higher than that (39%) in the yedoma and thermokarst deposits in arctic regions. In total, permafrost regions on the QXP contain approximately 160 ± 87 Pg SOC, of which approximately 132 ± 77 Pg (83%) stores in perennially frozen soils and deposits. Total organic carbon pools in permafrost regions on the QXP was approximately 8.7% of that in northern circumpolar permafrost region. The present study demonstrates that the total organic carbon storage is about 1832 Pg in permafrost regions on northern hemisphere.
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Perera, Duminda, Spencer Williams, and Vladimir Smakhtin. "Present and Future Losses of Storage in Large Reservoirs Due to Sedimentation: A Country-Wise Global Assessment." Sustainability 15, no. 1 (December 23, 2022): 219. http://dx.doi.org/10.3390/su15010219.

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Reservoir sedimentation is often seen as a site-specific process and is usually assessed at an individual reservoir level. At the same time, it takes place everywhere in the world. However, estimates of storage losses globally are largely lacking. In this study, earlier proposed estimates of sedimentation rates are applied, for the first time, to 47,403 large dams in 150 countries to estimate cumulative reservoir storage losses at country, regional, and global scales. These losses are estimated for the time horizons of 2022, 2030, and 2050. It is shown that 6316 billion m3 of initial global storage in these dams will decline to 4665 billion m3 causing a 26% storage loss by 2050. By now, major regions of the world have already lost 13–19% of their initially available water storage. Asia-Pacific and African regions will likely experience relatively smaller storage losses in the next 25+ years compared to the Americas or Europe. On a country level, Seychelles, Japan, Ireland, Panama, and the United Kingdom will experience the highest water storage losses by 2050, ranging between 35% and 50%. In contrast, Bhutan, Cambodia, Ethiopia, Guinea, and Niger will be the five least affected countries losing less than 15% of storage by 2050. The decrease in the available storage by 2050 in all countries and regions will challenge many aspects of national economies, including irrigation, power generation, and water supply. The newly built dams will not be able to offset storage losses to sedimentation. The paper is an alert to this creeping global water challenge with potentially significant development implications.
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Hunt, Julian David, Behnam Zakeri, Alexandre Giulietti de Barros, Walter Leal Filho, Augusto Delavald Marques, Paulo Sérgio Franco Barbosa, Paulo Smith Schneider, and Marcelo Farenzena. "Buoyancy Energy Storage Technology: An energy storage solution for islands, coastal regions, offshore wind power and hydrogen compression." Journal of Energy Storage 40 (August 2021): 102746. http://dx.doi.org/10.1016/j.est.2021.102746.

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35

Kaim, Barbara. "Storage Practices in the Merv and Serakhs Oases of the Partho-Sasanian Period." Ancient Civilizations from Scythia to Siberia 24, no. 1-2 (November 5, 2018): 440–66. http://dx.doi.org/10.1163/15700577-12341338.

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AbstractIn antiquity the oasis of Merv in the Murghab delta formed a relatively homogenous cultural region. At least from the Bronze Age onwards, the oasis shared a similar history with the neighbouring oasis of Serakhs in the ancient Tedjen delta. This paper focuses on storage practices in these two regions, drawing on recent archaeological work in the area which has revealed the existence of an array of methods for the storage and the administration of resources both in private dwellings and in official buildings. For a fuller picture, earlier storage practices and storage systems in these regions and neighbouring areas are first discussed, including specifically the area of the province of Parthia.
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Yülek, Murat Ali, İhsan Bostancı, and Koray Göksal. "Data Center Regions and Economic Development." International Journal of Social Ecology and Sustainable Development 8, no. 4 (October 2017): 32–47. http://dx.doi.org/10.4018/ijsesd.2017100103.

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The amount of data generated worldwide has reached unprecedented levels, and its rate of growth continues to increase exponentially. Brought about by rapid advances in information technologies, as well as changes in lifestyles and business strategies, this explosion in the quantity of data has given impetus to a fast-growing demand for data storage, which, in turn, has paved the way for large-scale data centers. This article addresses the potential economic impact of the construction of a “data center region” in a developing country, using as a case study a development project in Konya, Turkey. The core focus of the analysis is on whether such a data center region could create positive spillovers that trigger further development in a developing region.
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37

Hanaa H. Al-Saffar and Razzaq Shalan Augul. "Survey and revision of storage insects from several localities of Iraq." GSC Biological and Pharmaceutical Sciences 20, no. 3 (September 30, 2022): 175–86. http://dx.doi.org/10.30574/gscbps.2022.20.3.0351.

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Due to the importance of insects present in storages, which cause a lot of damage to stored materials (cereals, seeds, dates and other materials), the current study was proposed to determine the species spread in Iraq. It showed 31 species belonging to 16 genera under eight families and two orders. The specimens were collected from several storage spaces at several regions of Iraq. The species of Tribolium castaneum (Herbst, 1797) was most abundant population compared with other insects. The study also included a revision of the species that recorded previously in Iraq.
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38

Liu, Pei, Qiankun Wei, Zhongyuan Lin, and Wenbin Lv. "Optimized Schemes of “Infiltration”, “Storage”, and “Drainage” Measures against Urban Waterlogging in Plain River Network Regions." Water 14, no. 9 (April 24, 2022): 1381. http://dx.doi.org/10.3390/w14091381.

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Urban waterlogging has risen to be an urgent problem awaiting solutions in China these years, and “infiltration”, “storage”, and “drainage” are considered the major and most direct measures against this problem. In the present work, the waterlogging alleviation mechanism of these three measures is analyzed; and with Huangbian Village in Panyu District of Guangzhou, China, as a study case, one-dimensional, two-dimensional, and pipe network coupling hydrodynamic models were established to explore the optimal schemes of “infiltration”, “storage”, “drainage” measures against urban waterlogging and which measure is the most effective one, providing a reference for scientific prevention and alleviation of urban waterlogging in cities. Effect assessment shows that the “storage” is the most effective measure because reducing the impermeability near the waterlogged site, deploying storage tanks upstream of the waterlogged site, and in the case of submerged discharge, lowering the downstream water level can reduce the waterlogged area by 16%, 81%, and 16%, respectively. The comprehensive measures of “infiltration”, “storage”, and “drainage” reduced the waterlogged area by 87%, which is superior to a single measure. The present work is expected to provide some reference for the prevention and alleviation of urban waterlogging in cities on a plain with intensive river networks.
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39

Liu, Pei, Qiankun Wei, Zhongyuan Lin, and Wenbin Lv. "Optimized Schemes of “Infiltration”, “Storage”, and “Drainage” Measures against Urban Waterlogging in Plain River Network Regions." Water 14, no. 9 (April 24, 2022): 1381. http://dx.doi.org/10.3390/w14091381.

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Urban waterlogging has risen to be an urgent problem awaiting solutions in China these years, and “infiltration”, “storage”, and “drainage” are considered the major and most direct measures against this problem. In the present work, the waterlogging alleviation mechanism of these three measures is analyzed; and with Huangbian Village in Panyu District of Guangzhou, China, as a study case, one-dimensional, two-dimensional, and pipe network coupling hydrodynamic models were established to explore the optimal schemes of “infiltration”, “storage”, “drainage” measures against urban waterlogging and which measure is the most effective one, providing a reference for scientific prevention and alleviation of urban waterlogging in cities. Effect assessment shows that the “storage” is the most effective measure because reducing the impermeability near the waterlogged site, deploying storage tanks upstream of the waterlogged site, and in the case of submerged discharge, lowering the downstream water level can reduce the waterlogged area by 16%, 81%, and 16%, respectively. The comprehensive measures of “infiltration”, “storage”, and “drainage” reduced the waterlogged area by 87%, which is superior to a single measure. The present work is expected to provide some reference for the prevention and alleviation of urban waterlogging in cities on a plain with intensive river networks.
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40

Liu, Pei, Qiankun Wei, Zhongyuan Lin, and Wenbin Lv. "Optimized Schemes of “Infiltration”, “Storage”, and “Drainage” Measures against Urban Waterlogging in Plain River Network Regions." Water 14, no. 9 (April 24, 2022): 1381. http://dx.doi.org/10.3390/w14091381.

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Urban waterlogging has risen to be an urgent problem awaiting solutions in China these years, and “infiltration”, “storage”, and “drainage” are considered the major and most direct measures against this problem. In the present work, the waterlogging alleviation mechanism of these three measures is analyzed; and with Huangbian Village in Panyu District of Guangzhou, China, as a study case, one-dimensional, two-dimensional, and pipe network coupling hydrodynamic models were established to explore the optimal schemes of “infiltration”, “storage”, “drainage” measures against urban waterlogging and which measure is the most effective one, providing a reference for scientific prevention and alleviation of urban waterlogging in cities. Effect assessment shows that the “storage” is the most effective measure because reducing the impermeability near the waterlogged site, deploying storage tanks upstream of the waterlogged site, and in the case of submerged discharge, lowering the downstream water level can reduce the waterlogged area by 16%, 81%, and 16%, respectively. The comprehensive measures of “infiltration”, “storage”, and “drainage” reduced the waterlogged area by 87%, which is superior to a single measure. The present work is expected to provide some reference for the prevention and alleviation of urban waterlogging in cities on a plain with intensive river networks.
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41

Coffman, E. G., L. Flatto, I. Mitrani, L. A. Shepp, and C. Knessl. "Stochastic Models of Queue Storage." Probability in the Engineering and Informational Sciences 2, no. 1 (January 1988): 75–93. http://dx.doi.org/10.1017/s0269964800000644.

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We study a model of queue storage in which items (requests for single units of storage) arrive in a Poisson stream and are accommodated by the first available location in a linear scan of storage. The processing times of items are independent, exponentially distributed random variables. The set of occupied locations (identified by their indices) at time t forms a random subset Si, of [1,2,.…]. The extent of the fragmentation in Si, i.e., the alternating holes and occupied regions of storage, is measured by Wt, = max St, – |St|.
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42

Aljamaan, Hamza, Cynthia M. Ross, and Anthony R. Kovscek. "Multiscale Imaging of Gas Storage in Shales." SPE Journal 22, no. 06 (August 17, 2017): 1760–77. http://dx.doi.org/10.2118/185054-pa.

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Summary Four intact 2.54-cm-diameter cores from different shale plays (Barnett, Haynesville, Eagle Ford, and Permian Basin) were analyzed for their gas-storage capacity by use of a novel multiscale-imaging methodology spanning from centimeter to nanometer scale. Gas-storage (free and sorbed gas) capacity was investigated at the core scale with carbon dioxide (CO2) and krypton (Kr) by use of X-ray computed tomography (CT) with voxel dimensions of 190 × 190 × 1000 µm. Also, 2D tiled images were acquired with a scanning electron microscope (SEM) and stitched together to form 2.54-cm-diameter mosaics with a pixel resolution of 1.5 µm. Multiscale-image registration was then carried out to align the CT data with the SEM mosaics. Energy-dispersive spectroscopy (EDS) generated elemental spectra maps and subsequent component maps for regions with either substantial or minimal gas storage to assess the interplay of structural features (e.g., fractures) and matrix composition with respect to gas accessibility and storage. Registration of CT scans (vacuumed and gas-filled) as well as 190-µm-resolution CT-derived gas-storage maps with 1.5-µm-resolution SEM mosaics is straight forward for samples with dense features (such as calcite-filled fractures) that are resolvable by CT imaging. Alignment methods were developed for samples lacking these features, including registration marks by use of silver paint and intermediate-resolution microCT scans with cubic voxel dimensions of 27 µm. After alignment, the relationship of enhanced storage zones with open fractures and reduced storage regions with secondary mineralization (such as nodules) is apparent for the carbonaceous samples. For the clay-rich Barnett sample, fracture-filling calcite is associated with reduced storage similar to the other samples; however, secondary carbonate cementation within the clay matrix aligns with regions with substantial Kr- and CO2-gas storage. In contrast, clay-rich matrix regions lacking secondary carbonate cementation exhibit minimal gas-storage potential. Causes for this unexpected result include reduced gas accessibility and, possibly, low organic-matter content in the clay-rich matrix compared with secondary cemented matrix. These gas-sorption experiments prove the feasibility of dynamic core- to nanometer-scale CT/SEM/EDS image registration to improve sample characterization. To our knowledge, this is the first investigation of core-scale CO2-gas storage using multiscale imaging. CT and SEM image registration reveal spatial details regarding gas accessibility and storativity at the core scale. This work also supports the potential of carbon storage in shale formations and guides engineers toward optimal CO2-injection zones for enhanced gas recovery.
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WANG, Hua, Yu HUANG, Si-Long WANG, and Dong-Sheng ZOU. "Carbon and nitrogen storage under different forest ecosystems in mid-subtropical regions." Chinese Journal of Eco-Agriculture 18, no. 3 (May 18, 2010): 576–80. http://dx.doi.org/10.3724/sp.j.1011.2010.00576.

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44

Bott, Rubiana F., and Wanderley P. Oliveira. "Storage Conditions for Stability Testing of Pharmaceuticals in Hot and Humid Regions." Drug Development and Industrial Pharmacy 33, no. 4 (January 2007): 393–401. http://dx.doi.org/10.1080/03639040600975022.

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45

Kilpatrick, L. "Amygdala modulation of parahippocampal and frontal regions during emotionally influenced memory storage." NeuroImage 20, no. 4 (December 2003): 2091–99. http://dx.doi.org/10.1016/j.neuroimage.2003.08.006.

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46

Najjar, Yousef S. H., and Mahmoud S. Zaamout. "Performance analysis of compressed air energy storage (CAES) plant for dry regions." Energy Conversion and Management 39, no. 15 (October 1998): 1503–11. http://dx.doi.org/10.1016/s0196-8904(98)00034-x.

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47

Ferrucci, Franco, Driss Stitou, Pascal Ortega, and Franck Lucas. "Mechanical compressor-driven thermochemical storage for cooling applications in tropical insular regions." Energy Procedia 142 (December 2017): 3415–20. http://dx.doi.org/10.1016/j.egypro.2017.12.479.

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48

Chen, Yun, Juan P. Guerschman, Zhibo Cheng, and Longzhu Guo. "Remote sensing for vegetation monitoring in carbon capture storage regions: A review." Applied Energy 240 (April 2019): 312–26. http://dx.doi.org/10.1016/j.apenergy.2019.02.027.

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49

Bahadori, Mehdi N., and Fariborz Haghighat. "Long-term storage of chilled water in cisterns in hot, arid regions." Building and Environment 23, no. 1 (January 1988): 29–37. http://dx.doi.org/10.1016/0360-1323(88)90015-7.

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50

Lyashenko, V. I., V. I. Golik, and V. Z. Dyatchin. "Increasing environmental safety by reducing technogenic load in mining regions." Izvestiya. Ferrous Metallurgy 63, no. 7 (October 5, 2020): 529–38. http://dx.doi.org/10.17073/0368-0797-2020-7-529-538.

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One of the most problematic points in technology for storing ore enrichment waste materials with hardener admixture into underground mined space and tailing dumps are the tailings of hydrometallurgical plant (HMP). They are supplied through a slurry pipeline to the tailing dump in form of pulp with solid to liquid mass ratio of 1:2. Liquid phase of the pulp after gravity separation and clarification in tailing dump is returned to technological cycle of HMP. Storage technology under consideration has several disadvantages: high nonrecurrent capital costs for construction of tailing dump at full design capacity; high probability of harmful chemicals migration into groundwater if protective shields of the base or sides of tailings are damaged. The authors have used data from literature and patent documentation considering storage parameters, laboratory and production experiments, physical modeling and selection of compositions of hardening mixtures. Analytical studies, comparative analysis of theoretical and practical results by standard and new methods were performed. Possibility of using hardening mixtures with adjacent production wastes used as binders was established. Optimal composition of ingredients per 1 m3 of hardening mixture is proposed as follows: 1350 – 1500 kg of HMP tailings; 50 - 70 kg of binder (cement); 350 liters of mixing water. Proposed technology of ore enrichment waste storage into underground mined space and tailings with hardener admixture application allows using underground mined space at the enterprise production capacity of 1,500 thousand tons per year to store 50 – 55 % of tailings, and store the rest wastes cemented by binding material in repository. When filling the entire area of the tailing dump mirror of 10 m height with cemented tails and HMP capacity of up to 1.5 million tons per year, its operation life is extended by 50 years.
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