Thematische Bibliographien / Reservoirs on the Yellow Hill

Inhaltsverzeichnis

  1. Zeitschriftenartikel
  2. Dissertationen
  3. Bücher
  4. Buchteile
  5. Konferenzberichte
  6. Berichte der Organisationen

Auswahl der wissenschaftlichen Literatur zum Thema „Reservoirs on the Yellow Hill“

Autor: Grafiati
Veröffentlicht am 28. Juni 2021
Zuletzt aktualisiert am 1. Februar 2022

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Zeitschriftenartikel zum Thema "Reservoirs on the Yellow Hill"

1

Fu, Hong Jun. „Reservoir Characteristics of Buried Hill and Oil and Gas Distribution of Hailaer Basin - Case Study of Budate Formation of Sudeerte Oilfield“. Advanced Materials Research 926-930 (Mai 2014): 4425–28. http://dx.doi.org/10.4028/www.scientific.net/amr.926-930.4425.

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Buried hill reservoirs are typically found in Sudeerte oilfield in Hailaer basin. In this paper, the lithology, physical property and electric property of buried hill reservoirs are studied incorporating core data, mud logging, wireline logging and seismic attributes data. The major reservoir types of Budate buried hill are confirmed to include porosity, fracture, cavern and dissolved pore, which belong to dual porosity reservoirs. Vertically, the reservoirs get worse with the increase of buried depth and are controlled horizontally by weathering crust position and tectonic stress, and locations nearby fractured belt and structural high positions are preferable places for the formulation of good reservoirs. Oil and gas within the reservoir mainly accumulated inside fractures and pores and reservoirs with plenty existence of fractures and pores have good oil and gas shows and vice versa.
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Nie, Gui Min, Dan Guo, Yan Wang und Xiao Wei Cheng. „Research and Application of the Deep Horizontal Drilling and Completion Technology for Liaohe Oilfield Buried Hill Reservoir“. Applied Mechanics and Materials 241-244 (Dezember 2012): 1396–99. http://dx.doi.org/10.4028/www.scientific.net/amm.241-244.1396.

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With the depletion of shallow-layer oil and gas pools inLiaohe oilfield, buried hill stratigraphic reservoirs in Liaohe oil field are becoming main objectives for exploration in recent years, especially in high-risk areas of Xinglongtai deep the Hing ancient buried hill resources are particularly rich. Since 2007, Liaohe oilfield increased investment for Buried Hill reservoirs with deep horizontal drilling developt the buried hill reservoir. Liaohe has completed 36 deep horizontal, with a total footage of 183920m, the average depth of 5109m. Improving drilling speed of "buried hill deep horizontal and branch horizontal wells”, and reducing drilling costs are of great urgency. “Hing buried hill deep horizontal, horizontal wells,” with composite drilling technology, supporting the optimization of PDC bits, the high-pressure jet drilling, the MWD borehole trajectory control and optimization of drilling parameters, the new drilling fluid technology and so on. With a large number of horizontal wells put into Buried Hill stratigraphic reservoirs, oil and gas production of average deep horizontal well increase of 2-5 times. Besides, the previous recovery and production of oil and gas reservoirs significantly improved to create an objective economic and social benefits.
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Sun, Xue Lan, Chun Hong Hu und Jing Qi Xie. „Influence Analysis of Reservoirs on River Health“. Advanced Materials Research 368-373 (Oktober 2011): 1241–44. http://dx.doi.org/10.4028/www.scientific.net/amr.368-373.1241.

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Based on the current situation of the Lower Yellow River channel, this paper analyses the factors affecting river health, points out that river channel health is the foundation and key to river health. It evaluates the Yellow River's downstream channel health using fuzzy comprehensive evaluation method and gets the conclusion that the Yellow River's downstream channel health has deteriorated in 50 years and has improved in the beginning of this century. This paper analyses and points out that the reservoir to regulate natural flow-sediment process is the primary means that the human impact on river health. The regulation of reservoir has duality that "excessive" regulation will seriously damage river health and "moderate" regulation can better maintain and restore river health. Coordination of flow-sediment relationship is the key to maintaining the health of the Lower Yellow River.
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Xiu, Da. „Research on Reservoir Conditions of Buried Hill Reservoirs“. IOP Conference Series: Earth and Environmental Science 252 (09.07.2019): 052011. http://dx.doi.org/10.1088/1755-1315/252/5/052011.

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WANG, Jincai, Lun ZHAO, Xiangzhong ZHANG, Zhigang YANG, Haili CAO, Li CHEN, Fachao SHAN und Minghui LIU. „Buried hill karst reservoirs and their controls on productivity“. Petroleum Exploration and Development 42, Nr. 6 (Dezember 2015): 852–60. http://dx.doi.org/10.1016/s1876-3804(15)30082-3.

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Tian, Shimin, Yi Zhao, Yuanjian Wang, Enhui Jiang und Shoubing Yu. „Study on Ecological Scheduling of the Xiaolangdi Reservoir Based on the Ecological Needs of Estuarine Fishes“. MATEC Web of Conferences 246 (2018): 01045. http://dx.doi.org/10.1051/matecconf/201824601045.

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The total water amount into the Yellow River estuary is significantly reduced with the construction of a series of reservoirs in the Yellow River, which has a lot of adversely effects on the fishes and fishery resources in the estuary. This research analyzes the impacts of the reservoirs on the runoff and discharge in the Lower Yellow River and the estuary, and pays more attention to the influences of the reduction of water amount on the estuarine ecology and fishes. As a large reservoir nearest to the estuary in the Lower Yellow River, the operation of Xiaolangdi Reservoir plays an important role on the ecological restoration of the lower reaches of the Yellow River and the estuary. Two ecological operation schemes are proposed based on the ecological demands of the estuarine fishes and the actual operation of the Xiaolangdi Reservoir in recent years. One scheme is proposed only on the basis of the estuarine ecological water demands and another scheme takes consideration of ecological water demands and the actual status of the water resources in the Lower Yellow River synthetically. Finally, the feasibility of the two schemes are analyzed according to the actual situation of water storage of the reservoirs in the Yellow River in 2017.
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Wu, Jun Lai, Yue Tian Liu und Hai Ning Yang. „Parameters Optimization of Stereoscopic Horizontal Well Patterns by Using Numerical Reservoir Simulation“. Advanced Materials Research 433-440 (Januar 2012): 2602–6. http://dx.doi.org/10.4028/www.scientific.net/amr.433-440.2602.

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Well pattern is the most important affecting factor to the ultimate recovery for an oilfield development. Many researches are reported on areal well pattern, which is widely used in conventional reservoirs development such as low permeability reservoirs, heavy oil reservoirs, multi-layer sandstone reservoirs, etc. In this paper, according to the geological characteristics of fractured buried hill reservoir of Liaohe Oilfield, we firstly present the concept of stereoscopic well patterns and compare it with common areal water flooding. By using numerical reservoir simulation method, we design and optimize the parameters of 5-spot stereoscopic horizontal well patterns, including payzone thickness and horizontal well length under different anisotropic factors of fracture permeability. This can be successfully applied on the development of MM block fractured buried hill reservoir of Liaohe Oilfield.
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Burrows, V. D. „AC Hill oat“. Canadian Journal of Plant Science 72, Nr. 2 (01.04.1992): 439–41. http://dx.doi.org/10.4141/cjps92-050.

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AC Hill oat (Avena sativa L.) is a spring-type, daylength-sensitive, naked-seeded cultivar suitable for the feed and food industries in eastern Canada. It outperformed the check cultivar Tibor in yield, kernel size, hectolitre weight, and percentage of covered seeds in threshed grain. It is resistant to crown rust (Puccinia coronata Cd. f.sp. avenae Eriks. and E. Henn.) race CR13 but is equal to Tibor in loose smut (Ustilago avenae (Pers.) Rostr.) resistance, plant height and susceptibility to septoria (Septoria avenae Frank f.sp. avenae) blotch and barley yellow dwarf virus (BYDV). It is more susceptible to lodging and later in heading and maturity than Tibor.Key words: Avena sativa L., rust and smut resistance, cultivar description, naked oat
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Zhang, Tingting, Ruifeng Zhang, Jianzhang Tian, Lifei Lu, Fengqi Qin, Xianzeng Zhao und Yuefeng Sun. „Two-parameter prestack seismic inversion of porosity and pore-structure parameter of fractured carbonate reservoirs: Part 2 — Applications“. Interpretation 6, Nr. 4 (01.11.2018): SM9—SM17. http://dx.doi.org/10.1190/int-2018-0019.1.

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Fractures and fracture-related dissolution pores, as well as cavities, molds, and vugs, provide the major conduit and/or storage space for hydrocarbons in the deeply buried carbonate hill of Hexiwu field, Bohai Bay Basin. The fractured reservoir generally has lower porosity but better permeability than moldic/vuggy reservoir, and it consists of the major part of the buried-hill slope and buried-hill internal reservoirs. The conventional method of characterizing carbonate reservoirs, however, often mixes these two types of reservoirs together because they both have low acoustic impedance and low bulk modulus. The rock-physics analysis of two field wells indicates that a pore-structure parameter defined in a rock-physics model, the so-called Sun model, can help to distinguish the fractured reservoir zones together with porosity. Fractured zones usually have porosity of less than 5% and a pore-structure parameter of greater than six, whereas moldic/vuggy reservoirs of higher porosity have a pore-structure parameter of less than six. Field-scale application demonstrates that simultaneous prestack seismic inversion for the porosity and pore-structure parameter enables 3D mapping of fractured reservoir zones in the buried carbonate hills. It also provides an analog of detecting fractures and/or fracture-related pores in deeply buried carbonates in similar geologic settings.
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Ragab, R., D. Moidinis, J. Albergel, J. Khouri, A. Drubi und S. Nasri. „The HYDROMED model and its application to semi-arid Mediterranean catchments with hill reservoirs 2: Rainfall-runoff model applications to three Mediterranean hill reservoirs“. Hydrology and Earth System Sciences 5, Nr. 4 (31.12.2001): 554–62. http://dx.doi.org/10.5194/hess-5-554-2001.

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Abstract. The objective of this work was to assess the performance of the newly developed HYDROMED model. Three catchments with hill reservoirs were selected. They are El-Gouazine and Kamech in Tunisia and Es Sindiany in Syria. The rainfall, the spillway flow and volume of water in the reservoirs were used as input to the model. Events that generated spillway flow were preferred for calibration. The results confirmed that the HYDROMED model is capable of reproducing the runoff volume at all the three sites. In calibrating single events, the model performance was high as measured by the Nash-Sutcliffe criterion for goodness of fit. In some events this value was as high as 98%. In simulation mode, the highest Nash-Sutcliffe criterion value was close to 70% in the El-Gouazine and Kamech catchments and close to 50% in the Es Sindiany catchment. Given the limited information available, especially on the unrecorded releases in the three catchments, the hydrological impact of site geology (e.g. Kamech), the unrecorded operator intervention during the spillway flow (e.g. Es Sindiany) and other unaccounted factors (e.g siltation, evaporation, etc.), these results are by and large very encouraging. However, they could be further improved as and when more information on the unrecorded parameters becomes available. Additionally, the results of this work highlighted the need for long term records with a large number of significant events that are able to generate spillway flow to obtain more consistent and reliable parameter values. It also highlights the need for more accurately recorded releases for irrigation and other uses. As these results are encouraging, more tests on those three and other sites are planned. Keywords: HYDROMED, rainfall-runoff model, Mediterranean, conceptual model
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Dissertationen zum Thema "Reservoirs on the Yellow Hill"

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Crouch, Ryan T. „Adding value to upground drinking water reservoirs: what makes a good yellow perch (Perca flavescens) fishery?“ Bowling Green State University / OhioLINK, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1291841439.

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Bücher zum Thema "Reservoirs on the Yellow Hill"

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Cummings, Dave. Periodic dam safety inspection report: College Hill, Beacon Hill reservoirs, first periodic inspection report. Olympia, Wash: Water Resources Program, Dam Safety Office, Washington State Dept. of Ecology, 2000.

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Cummings, Dave. Periodic dam safety inspection report: Beacon Hill (North) Reservoir. [Olympia, Wash.]: Washington State Dept. of Ecology, 2007.

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Dycus, Donald L. PCB studies on fish from Watts Bar, Fort Loudoun, Tellico, and Melton Hill Reservoirs - 1988. Chattanooga, Tenn: Tennessee Valley Authority, Resource Development, River Basin Operations, Water Resources, 1990.

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Dycus, Donald L. PCB studies on fish from Watts Bar, Fort Loudoun, Tellico, and Melton Hill Reservoirs - 1988. Chattanooga, Tenn: Tennessee Valley Authority, Resource Development, River Basin Operations, Water Resources, 1990.

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Butler, M. D. Yellow toadflax and Dalmatian toadflax, Linaria vulgaris Hill and Linaria dalmatica [L.] Mill. [Corvallis, Or.]: Oregon State University Extension Service, 1994.

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Yellow Boatie on Blue Hill Bay. Wooden Boat Publications, 2008.

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Yellow Rose Bride (Steeple Hill Cafe). Steeple Hill, 2006.

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Custodian of Yellow Point : The Biography of Gerry Hill. Beach Holme Publishers, Limited, 1991.

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McCauslin, Debra Sandoe. Reconstructing the Past: Puzzle of the Lost Community at Yellow Hill. BookSurge Publishing, 2007.

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Buchteile zum Thema "Reservoirs on the Yellow Hill"

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Yiying, Qian. „Effects and Significance of Water and Sediment Regulation by Reservoirs in the Middle Yellow River“. In The GeoJournal Library, 597–616. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2450-5_38.

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„Yellow dust“. In Clouds above the Hill, 217–64. Routledge, 2013. http://dx.doi.org/10.4324/9780203068724-19.

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Haugh, B. „Turlough Hill – Upper Reservoir: condition of the lining after 30 years“. In Reservoirs in a Changing World, 431–43. Thomas Telford Publishing, 2002. http://dx.doi.org/10.1680/riacw.31395.0034.

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Li, X., L. Sun und X. Meng. „Implement water diversion measures to ease the ecological water demand of the Yellow River Delta“. In Dams and Reservoirs under Changing Challenges, 829–33. CRC Press, 2011. http://dx.doi.org/10.1201/b11669-105.

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Hardy, Thomas. „Chapter II Night: the flock: an interior: another interior“. In Far from the Madding Crowd. Oxford University Press, 2008. http://dx.doi.org/10.1093/owc/9780199537013.003.0004.

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It was nearly midnight on the eve of St Thomas’,* the shortest day in the year. A desolating wind wandered from the north over the hill whereon Oak had watched the yellow waggon and its occupant in the sunshine of a few...
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Crouch, Dora P. „Eastern Grego-Roman Cities“. In Geology and Settlement. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780195083248.003.0011.

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Only since the last two decades of the twentieth century have professional geologists been working specifically at Miletus, investigating the shiny white limestone on top at KalabakHill; the limestone of Theater Hill and Humei Hill; and the limestone of Zeytin Hill (at the west of the hill called Degirmen, west of Kalabak), with sandstone and tuff to the east. The stratigraphy at Miletus is as follows, beginning with the topmost modern layer: . . . Iron deposits in mountains east of Miletus and both iron and brown coal at Mt. Mykale (today Samsun Dag) north of the Meander River valley. Volcanic tuff. Soluble limestone: 200 m of Yatagan or Balat strata of marble with tufa, sand, and gravel from which springs emerge. Early Pliocene limestone, shiny white limestone cap 60–100 m thick, karstified but with few on-site springs, forming ridges, hills, and a thick layer of scree. Miocene marls, sandstones, conglomerates, and clays with springs. Pink-yellow sandstone, sometimes with tuff, around sides of hills. Older clayey limestone deposited in a lake environment. Former large bay, now a swampy river plain with rich alluvial soil. . . . Prof. B. Schröder and his team have done geological research in the area (1990–94) and published their findings swiftly, which I acknowledge with gratitude. Suspected faults run north and south of Kalabak Hill (recognized in C. Schneider 1997). The town of Akköy to the south, where the German archaeological house is located well above the mosquitoes of the archaeological site in the swampy plain, sits on limestone that forms a peninsular ridge, surrounded on three sides by sandstone with tuff. The west coast of Asia Minor is subject to strong relief, steep gradients, and high precipitation; the high amount of energy available allows rapid change in topography (Gage 1978: 621). In Ionia, on average, the sea has risen or the land has sunk 1.75 m since antiquity (Bintliff 1977: 24; 1992). The Greek cities of Asia Minor were without exception built on or next to karst terrain (V. Klemes, 1988, personal communication when he was president of the International Association for Karst Hydrology).
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Hector, Scott, Karen Blake und Tim Elam. „Petroleum occurrences in the Mount Diablo area, California“. In Regional Geology of Mount Diablo, California: Its Tectonic Evolution on the North America Plate Boundary. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.1217(06).

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ABSTRACT Mount Diablo is flanked on its northeast side by a thick section of Late Cretaceous and Tertiary sedimentary rocks, which produced small hydrocarbon accumulations in the Los Medanos, Willow Pass, Mulligan Hill, and Concord gas fields. The first well was drilled in 1864, and today most of the active wells on the northeast flank are used for gas storage by Pacific Gas and Electric Company. These fields, which also include the Brentwood oil field, lie to the northeast of Mount Diablo and have produced 6.4 million cubic meters (225 billion cubic feet) of natural gas and over 57 million cubic meters (9.1 million barrels) of oil. The main reservoirs for the Sacramento Basin are sandstones in the Late Cretaceous and Paleogene section. The source rock there is primarily from the Upper Cretaceous Dobbins Shale, which began generation 75 m.y. ago, and the Winters Shale, which began generation 35 m.y. ago. The Livermore Basin is located on the western and southwestern sides of the mountain. The only commercial field in that basin is the small Livermore oil field. This field produces primarily from Miocene sandstones. The Livermore Basin is a Neogene basin that was syntectonically formed in the last few million years and continues to grow today. Studies of the black oils found in the Livermore field show that the source rock is likely the Eocene Nortonville Shale, though the Upper Cretaceous Moreno shale is also considered to be a possible source. The Livermore field has produced 12 million cubic meters of oil (1.9 million barrels).
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„Distribution of Yellow Perch Perca fl avescens in Lakes, Reservoirs and Rivers of Alberta and British Columbia, in Relation to Tolerance for Climate and other Habitat Factors, and their Dispersal and Invasive Ability“. In Biology of Perch, 83–110. CRC Press, 2015. http://dx.doi.org/10.1201/b18806-7.

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„up to 5-10 cm, without leaves. Corolla pale blue, 6-7 mm in diam., limb flat, with ovate-orbicular lobes, tube short, as long as calyx; arches on throat white or yellow, broad, papillate, forming crown, sealing tube inlet; after anthesis, style not projecting from calyx. Calyx campanulate, 2-2.5 mm long in flower, 3.5-5 mm long in fruits and pubescent with appressed bristles, incised for 1/3 into broad deltoid teeth. Fruit stems long, strong, 0.5-0.8 cm long, horizontally declinate in fruits, pubescent with appressed tiny bristles. Erema 1.5-1.7 mm long, brown, lustrous, ovate, with narrow wing; areola broad, trapezoidal, wit h short groove along margin. On Putoran plateau (Talnakh settlement) and in East. Sayan (Tunkinsk mountain range), 2 n = 22. Plate XVII (1). In swamps, humid meadows, along banks of water reservoirs in forest and forest-steppe regions. West. Sib.: TYU—Yam, Khm, Tb, KU, OM, TO, NO, KE, AL—Ba, Go. Cen. Sib,: KR—Ta, Pu, Tn, Kha, Ve, TU. East. Sib.: IR—An, Pr, BU—Se, Yuzh (Selenginsk region: Bichura village), YAK—Vi, Al.—Europe, Caucasus, Mid . Asia, Asia Minor, Nor. America. Described from Europe. Map 82.“ In Flora of Siberia, Vol. 11, 144–57. CRC Press, 2006. http://dx.doi.org/10.1201/9781482279696-26.

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Konferenzberichte zum Thema "Reservoirs on the Yellow Hill"

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Liu, He, Danfeng Xiao, Cunrong Li, Qi Liu, Changming Zhao, Wenming Huang und Minghui Zhang. „Optimized Fracturing Engineering Design for Buried Hill Reservoirs“. In Asia Pacific Oil and Gas Conference & Exhibition. Society of Petroleum Engineers, 2009. http://dx.doi.org/10.2118/121016-ms.

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Chun, Wang, Zhang Yan, Wu Xiaozhou, Li Wenke und Yu Tianyu. „Research of Strike-slip Faults Control Action on Buried Hill Reservoirs With Yannan Buried Hill Zone as An Example“. In SPG/SEG 2016 International Geophysical Conference, Beijing, China, 20-22 April 2016. Society of Exploration Geophysicists and Society of Petroleum Geophysicists, 2016. http://dx.doi.org/10.1190/igcbeijing2016-042.

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Yue, Yixing, Jin Pang, Hong Liu, Xu Zhang und Guijuan Pan. „Configuration Optimization Research on Tridimensional Injection-production Well Patterns of Buried Hill Reservoirs“. In 2015 International Conference on Mechatronics, Electronic, Industrial and Control Engineering. Paris, France: Atlantis Press, 2015. http://dx.doi.org/10.2991/meic-15.2015.361.

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Lyu, X. M., L. Yang, R. H. Wang, W. H. Guo, Q. F. Han und Z. C. Li. „A Case Study on Multiple Stratigraphic Reservoirs Related with Weathered Granite Buried-hill“. In 78th EAGE Conference and Exhibition 2016. Netherlands: EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201600694.

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Hadjerioua, Boualem, Katherine F. Lindquist und Vernon Siler. „Linking TVA's Norris and Melton Hill Reservoirs Water Quality -- CE-QUAL-W2 Models“. In World Water and Environmental Resources Congress 2001. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40569(2001)141.

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Wenjuan Yang, Qiang Huang, Yujie Lv und Yimin Wang. „Risk analysis of compensating regulation of cascade reservoirs on the main stream of yellow river“. In 2008 7th World Congress on Intelligent Control and Automation. IEEE, 2008. http://dx.doi.org/10.1109/wcica.2008.4592881.

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Zhang, Yinguo, Qinghua Chen, Qinghua Chen, Qinghua Chen, Jianwen Chen, Jianwen Chen, Jianwen Chen, Jianqiang Wang, Jianqiang Wang und Jianqiang Wang. „TYPES OF UNCONFORMITY AND PREDICTION OF HYDROCARBON RESERVOIRS IN YANTAI DEPRESSION, SOUTH YELLOW SEA BASIN“. In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297348.

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Lyu*, Ximin, Li Yang, Weihua Guo, Ronghua Wang und Qianfeng Han. „Multiple Stratigraphic Reservoirs Related With Weathered Granite Buried-Hill in Betara Uplift, South Sumatra Basin, Indonesia“. In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2204584.

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Zhou, Feng-Ming, Zhao-Wei Si, Fa-Wu Lin, De-Fang Liu, Hong Yang, Da-li Wang, Xian-Ran Zhao, Ping Yan, Guo Wei und Hai-Peng Zhao. „Prediction of Buried-Hill Productive Carbonate Reservoirs Using Electrical and Acoustic Image Logs, Ordovician Formation, China (II)“. In SPE Asia Pacific Oil and Gas Conference and Exhibition. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/165743-ms.

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Zhou, Feng-Ming, Zhao-Wei Si, Fa-Wu Lin, De-Fang Liu, Da-Li Wang, Xian-Ran Zhao und Ping Yan. „Prediction of Buried-Hill Productive Carbonate Reservoirs Using Electrical and Acoustic Image Logs, Ordovician Formation, China (I)“. In Unconventional Resources Technology Conference. Society of Exploration Geophysicists, American Association of Petroleum Geologists, Society of Petroleum Engineers, 2013. http://dx.doi.org/10.1190/urtec2013-279.

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Berichte der Organisationen zum Thema "Reservoirs on the Yellow Hill"

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Dycus, D. L. PCB studies on fish from Watts Bar, Fort Loudoun, Tellico, and Melton Hill Reservoirs, 1988. Office of Scientific and Technical Information (OSTI), September 1990. http://dx.doi.org/10.2172/6326338.

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Tomaszewski, T. M., D. J. Bruggink und D. L. Nunn. Report on water quality, sediment and water chemistry data for water and sediment samples collected from source areas to Melton Hill and Watts Bar reservoirs. Office of Scientific and Technical Information (OSTI), August 1995. http://dx.doi.org/10.2172/569066.

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Tomaszewski, T. M., D. J. Bruggink und D. L. Nunn. Summary report on water quality, sediment and water chemistry data for water and sediment samples collected from source areas to Melton Hill and Watts Bar reservoirs. Office of Scientific and Technical Information (OSTI), August 1995. http://dx.doi.org/10.2172/485959.

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