Artículos de revistas: "Sandy"

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Thevanayagam, S., T. Shenthan, S. Mohan y J. Liang. "Undrained Fragility of Clean Sands, Silty Sands, and Sandy Silts". Journal of Geotechnical and Geoenvironmental Engineering 128, n.º 10 (octubre de 2002): 849–59. http://dx.doi.org/10.1061/(asce)1090-0241(2002)128:10(849).

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2

Kryvulchenko, Anatolii. "Oleshkivski Sands as a hierarchically built natural system". Visnyk of the Lviv University. Series Geography 53 (18 de diciembre de 2019): 197–209. http://dx.doi.org/10.30970/vgg.2019.53.10666.

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Оleshkivski Sands (Oleshia) are one of the morphosculptures on the Left bank of the lower part of Dnipro river, which is formed on alluvial and periglacial deposits. The article clearly identifies the location of these sands among other morphosculptures of the Left bank of the lower part of Dnipro. In view of the ambiguity, two regions of the Left Bank are considered separately – nearby arenian sandy-loamy geocomplexes with the presence of extremely specific sandy hilly-depressions geocomplexes and the territory of the hilly-lowland plain (Kardashynka lowland), which is located between the Dnipro delta and sands massives of the Kelegei arena. Oleshia consists of seven hilly-sanded arenas and six inter-arenial sanded flat plains. Accordingly, the area of Оleshkivski Sands is 219.9 thousand hectares, almost 80 % of which are sanded arenas. Arenas are represented here as hilly sandy plains and depressions. These sandy plains divided by sand types such as hilly (hillock, hillock-dune and hilly), hilly-ridge and flat-wavy, depressions – by flat-wavy, ridge-hollow, wavy-shallow depressions and ridge-shallow depressions. Such types of relief forms are represented by the following microforms of aeolian genesis: hillocks, hills, parabolic dunes, aeolian fields, deflation depressions and also by microforms of fluvial genesis: hilly-ridges, depressions among hilly sandy massifs, gally (redundans), inter-ridge depressions (inter-ridge hollows). On the surface of sandy massifs, especially in places where the sands are exposed, relief nanoforms are formed, which are represented by small riffles, nabkhas, blowing furrows, tafonies and also by aeolian trains, cut-off lobes, cliffs, cornices. This system of forms of relief of the Oleshkivski Sands testifies to the complex and various processes of their formation, but special attention should be paid at sand ridges, especially those with the parallel ridge-hollow spatial organization. They, for example, in the south of the Kinburn arena became the basis for the formation of the aeolian-hydrogen landscape that is unique for the territory of Ukraine. The author associates the creation of the Oleshіa ridge-hollow geocomplexes with the probable catastrophic floods (floodstreams). It is advisable to consider these ridges as a manifestation of giant ripples (diluvial dunes), which are often covered by deposits with different nature of formation. This is evidenced by the variety of typology of relief forms on the territory of the Oleshkivski arenas. Thalassogenic, suffusion-subsidence and anthropogenic factors also deserve special attention in characterizing of shaping the relief of the region. Key words: the Left bank of the Lower Dnipro, Оleshkivski Sands, hierarchy of relief forms, sandy arena, aeolian processes, fluvial forms.

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3

Dulepova, N. A. y A. Yu Korolyuk. "Psammophyte vegetation of the Selenga river basin (Republic of Buryatia)". Vegetation of Russia, n.º 27 (2015): 78–95. http://dx.doi.org/10.31111/vegrus/2015.27.78.

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Modern aeolian relief is widespread in the forest-steppe landscapes of Transbaikalia. Valleys of the Selenga River and its inflows are the areas covered by ancient sandy deposits. Human impact in dry climatic conditions causes intensive wind erosion and formation of open and moving sands covered with sparse plants. The flora and vegetation of such landscapes notably differ from surrounding territories. It’s particularity is caused by presence and domination of plant species usually seen on open sands. Despite of numerous publications describing the sandy dunes of Transbaikalia, the psammophyte vegetation and natural dynamics of sandy landscapes are poorly documented. This study presents the analysis of 398 relevés describing psammophyte vegetation from the South-West Transbaikalia (Selenginsky, Dzhidinsky, Kyakhtinsky and Bichursky administrative disticts of the Republic of Buryatia).

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4

Aronsohn, Richard B. "“Sandy”". American Journal of Cosmetic Surgery 14, n.º 2 (junio de 1997): 208. http://dx.doi.org/10.1177/074880689701400222.

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5

Udoh, B. T. y T. O. Ibia. "Fertility capability classification for agricultural land use planning in the beach sands area of Akwa Ibom State, Nigeria". Agro-Science 21, n.º 2 (22 de junio de 2022): 74–78. http://dx.doi.org/10.4314/as.v21i2.8.

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Soil survey and fertility capability classification (FCC) were carried out in an area mostly underlain by the beach ridge sands (BRS) parent material in Akwa Ibom State, Nigeria. The study applied the FCC in agricultural land use planning for efficient land management and optimal agricultural productivity of the beach soils. Field and laboratory data were obtained from 40 pedons located across eight Local Government Areas on the BRS parent material. From the results of field and laboratory studies, 11 FCC units were identified in the area. Based on similarities in certain soil profile characteristics, the 11 FCC units were grouped into four agro-ecological units (AEUs): (i) poorly drained FCC units with sandy topsoil over sandy subsoil, grouped to form AEU-A, covered 65.00% of study area; (ii) well drained FCC units with sandy topsoil over sandy subsoil, formed AEU-B and covered 22.50% of study area; (iii) poorly drained FCC units with sandy topsoil over loamy subsoil or loamy top- and sub- soils, formed AEU-C and covered 7.50% of study area; (iv) well drained FCC units with sandy topsoil over loamy subsoil, which formed AEU-D, occupied 5.00% of study area. The result of this study has shown that FCC can be employed as a simple but efficient tool in agricultural land use planning. Major soil profile characteristics used to differentiate land units within the beach sands area of Akwa Ibom State are drainage and texture.

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6

Syvyj, M. y B. Gavrychok. "Construction sands of Podillya: patterns of distribution, resources and use". Journal of Geology, Geography and Geoecology 27, n.º 3 (8 de enero de 2019): 510–19. http://dx.doi.org/10.15421/111875.

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This article presents the characteristics of the resource base of building sands within the three Podillya regions, the patterns of sands distribution, and proposals for increasing the extraction of raw materials . The construction sands of Podillya are confined to the Upper Cretaceous, Neogene and Anthropogenicdeposits. The decrease of the thickness of the sandy strata of the Opilsk Neogene suite in the eastern direction was observed with the simultaneous increase in the thickness of the overlapping strata of the rocks. There is no apparent correlation between the thickness of sandy interlayers and the quality of sands. The interdependence of the chemical composition of Neogene sands and the sand size module is established.The genetic predisposition for the distribution of building sands in different parts of the Podillya territory has been established. Four groups of sand deposits of different age have been identified within the Podillya regions, which contrast sharply with single deposits in the neighbouring territories.There is a very uneven distribution of explored reserves of sandy raw materials across the region and accordingly in the provision of construction sands in the different oblasts /regions of Podillya. The areas best provided with sandy raw materials are the central districts of Ternopil region and Slavutsky district of Khmelnytsky region . Sands of the Baltic stage distributed in Vinnytsia region are mostly poor in quality, clogged with clay material and require enrichment. The further development of the mineral raw material base and the prospects for increasing the production of construction sand in the Podillya regions is associated with the increase in production at the prepared deposits, the commissioning of reserve deposits, the conducting of prospecting and exploration work in the proposed potentially exploitable areas and additional exploration of individual deposits that are exploited. The research allows us to evaluate objectively the existing base of sand raw materials for various purposes in the Podillya region and to develop on this basis measures to increase it. The importance of the study is determined by the acute shortage of the raw material in most administrative districts of Khmelnytsky and Vinnytsia regions, by the growth in the volume of construction work (and accordingly the requirements for sandy raw materials) both in Podillya and in the country.

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7

Bulokhov, A. D. y A. M. Petrenko. "Communities of the class Koelerio-Corynephoretea Klika in Klika et Novák 1941 in the Bryansk region of Russia". Vegetation of Russia, n.º 30 (2017): 29–34. http://dx.doi.org/10.31111/vegrus/2017.30.29.

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Only few publications on the classification of vegetation of Koelerio–Corynephoretea canescentis Klika in Klika et Novák1941 class, that unites pioneer communities on sandy soils, dunes or an exposed sands, is known for Bryansk region of Russia (Bulokhov, 2001; Bulokhov, Kharin, 2008). This region is located in the western part of the East European plain, on the watershed of two large river (Dnieper and Volga) systems, occupying the central part of the Desna river pool and the woody watershed between Desna and Oka. The territory (34.9 thousand кm2) is extended from the west to the east on 270 km (between 31°10′ and 35°20′ E) and from the north to the south — on 190 km (between 54°05′ and 52°10′ N). The main item of this paper is to submit the results of the classification carried out upon thebasis of 57 releves made in 2003–2016 in Bryansk region and to characterize the composition, distribution and syntaxonomical position of thepioneer vegetation of sandy and shallow soils communities within it. Three new associations are described according to Braun-Blanquet floristic classification. The syntaxon nomenclature of the higher ranks follows Mucina et al. (2016) The ass. Thymo serpylli–Koelerietum glaucae ass. nov. hoc loco, with synecological optimum on dry poor sandy soils, is diagnosed by character species Artemisia campestris, Koeleria glauca, Thymus serpyllum. Its communities occur on fringes of the lichen pine forests, sandy river terraces and outwash plains. Two subassociations are distinguished within the association: T. s.–K. g. typicum (with var. typica and Corynephorus canescens) and agrostietosum vinealis subass. nov. hoc loco (with var. typica and Calluna vulgaris) with Agrostis vinealis, Dianthus arenarius, Cladonia arbuscula as differential species. The ass. Koelerio glaucae–Plantaginetum arenariae ass. nov. hoc loco, with synecological optimum on dry poor sandy soils or exposed sands, is diagnosed by Plantago arenaria and Koeleria glauca. Its communities occuron the exposed sands, fringes of lichen pine forests and not flooded sandy river crests. The ass. Diantho borbasii–Festucetum polesicae ass. nov. hoc loco with synecological optimum on dry, weekly acidic, poor of mineral nitrogen, sandy soils or the exposed sands, is diagnosed by Festuca polesica, Astragalus arenarius, Jurinea cyanoides, Otites parviflora. Communities occur on the exposed sands, fringes of lichen pine forests. Two variants are distinguished within association: Sempervivum ruthenicum (on dunes with dry, poor, weekly developed soils) and typica. These three associations are the early stages of the progressive succession of oligotrophic lichen pine forests on the river terraces or of the heath meadows in flood river plains.

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8

Thevanayagam, S., K. Ravishankar y S. Mohan. "Steady-State Strength, Relative Density, and Fines Content Relationship for Sands". Transportation Research Record: Journal of the Transportation Research Board 1547, n.º 1 (enero de 1996): 61–67. http://dx.doi.org/10.1177/0361198196154700109.

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The appropriate choice of shear strength of liquefied sands is an important component in seismic slope stability evaluation. Several factors affect the undrained steady-state strength (Sus) of sands. The steady-state strengths of 24 sandy soils were analyzed. It is shown that fines content, relative density, and friction angle play important roles affecting Sus. Fines content was found to be the major factor affecting Sus. This was verified experimentally for one sand. When the Sus. data for sands were grouped into (a) relatively clean sands (<12 percent fines), (b) silty sands (12 to 50 percent fines), and (c) silts or sandy silts (>50 percent fines), at the same relative density, relatively clean sands showed the highest Sus. Silts showed the lowest Sus. Silty sands showed intermediate strengths. Lower-bound Sus-relative density relationships were established for relatively clean sands and silty sands.

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9

Rogerson, Andrew, Fiona Hannah, Gwen Hauer y Phillip Cowie. "Numbers of naked amoebae inhabiting the intertidal zone of two geographically separate sandy beaches". Journal of the Marine Biological Association of the United Kingdom 80, n.º 4 (agosto de 2000): 731–32. http://dx.doi.org/10.1017/s0025315400002563.

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Numbers of naked amoebae (Gymnamoebae) inhabiting the lower intertidal zone of two sandy beaches were estimated using a novel enrichment cultivation method. Samples were collected between June and September, 1999. Beach sand at Kames Bay, Isle of Cumbrae, Scotland contained on average 2604 amoebae cm−3 while at Dania Beach, Florida, USA, sand harboured 4236 amoebae cm−3. This is the first study to focus on the abundance of naked amoebae inhabiting a sandy beach. These numbers are higher than densities generally reported for shallow subtidal sands and show that amoebae must be considered in future studies on the dynamics of sandy beach communities.

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10

Amador, Elmo Da Silva. "Geologia e Geomorfologia da Planície Costeira da Praia do Sul: Ilha Grande - Uma Contribuição à Elaboração do Plano Diretor da Reserva Biológica". Anuário do Instituto de Geociências 11 (1 de enero de 1987): 35–58. http://dx.doi.org/10.11137/1987_0_35-58.

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Based on stratigraphical, sedimentological and geomorphological methods, a preliminary stratigraphic division is proposed to the Praia do Sul coastal plain, a state Biological Reserve, located in "Ilha Grande", Rio de Janeiro. This reserve was created to preserve the natural ecosystems found therein (sandy coastal plain, mangrove, lagoon, rocky coast and hillside fo rest). The Praia do Sul sedimentation plain is essentially constituted by continental gravels and sands of Upper Pleistocene, marine sandy formations, fluvial-lagoonal sandy-clayer formations and present mangrove swamps and beachs. The paleogeographic evolution of this area can be followed through the sedimentary association that permits to establish the transgressive and regressive process that occured during the Quaternary period.

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11

Toé Bi, Kizito Katel Kahou, N’goran Jean-Paul Yao, Touvalé Marcel Kessé y Zéli Bruno Digbéhi. "Caracterisation Sedimentologique Et Hydrodynamique Des Formations Sableuses Du Miocene Inferieur De La Region D’eboinda (Sud-Est De La Cote d’Ivoire)". European Scientific Journal, ESJ 12, n.º 9 (30 de marzo de 2016): 192. http://dx.doi.org/10.19044/esj.2016.v12n9p192.

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Five hundred and five (505) cuttings samples of 51 survey (of 10 m depth maximum) drilled in Eboinda area (South-western of Côte d’Ivoire) were subject to lithological, mineralogical an granulometry studies in order to clarify the nature of sediments and factors and processes involved during their transport and deposition. The "Surfer" software helps to map the formations. The results indicate: - lithologically:, six mains facies were defined ; sandy clays with gravel, clayey sand, sands, siltyey clay, sandy clays and clay. Sandy sediments were mapped to north and clayed one in south of the study area. Most of studied sands were interpreted as river and coastal dune deposits. Many minerals were described such as sphene, zircon, tourmaline, ilmenite, hematite, apatite, limonite, sillimanite, chromite, muscovite, garnet, chlorite, rutile, goethite, quartz and feldspar. The clay fraction is composed by kaolinite, quartz, apatite, gypsum, goethite and halloysite; - hydrodynamically: the surfacecreep is the main mode of transport expressed within units III and VI. While saltation characterizes sand units IV and V. Predominance of rounded forms and sub-rounded features of quartz grains suggests a transport in aqueous zone over a long distance. In the other hand the sands of units VI and III are essentially sub-angular, suggesting a close generating source. The blunt and shiny aspect of most sands grains encountered, confirm the mode of transport in aqueous zone.

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12

Qualls, Larry. "Sandy Skoglund". Performing Arts Journal 16, n.º 1 (enero de 1994): 102. http://dx.doi.org/10.2307/3245831.

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13

Ahmadi, Ramin. "Sandy Hook". Annals of Internal Medicine 158, n.º 3 (5 de febrero de 2013): 218. http://dx.doi.org/10.7326/0003-4819-158-3-201302050-00017.

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14

Pollak, Cheryl L. ""Hurricane" Sandy". Texas A&M Journal of Property Law 5, n.º 2 (diciembre de 2018): 157–92. http://dx.doi.org/10.37419/jpl.v5.i2.3.

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On the evening of October 29, 2012, “Hurricane” Sandy made land- fall on the New York coastline, battering the land with strong winds, torrential rain, and record-breaking storm surges. Homes and commercial structures were destroyed; roads and tunnels were flooded; and more than 23,000 people sought refuge in temporary shelters, with many others facing weeks without power and electricity. At the time, Sandy was heralded as one of the costliest hurricanes in the his- tory of the United States; the second costliest hurricane only to Katrina, which hit New Orleans in 2005. Unfortunately, recent experience with Hurricanes Florence, Maria, Harvey, and Irma suggest that this pattern of devastating superstorms may become the new norm as climate change produces more extreme and unpredictable weather events. In Sandy’s aftermath, as individuals returned to their homes, or what remained of them, and communities began to rebuild, the true cost of the storm became apparent. A year after the storm, the Federal Emergency Management Agency (“FEMA”) estimated that over $1.4 billion in assistance was provided to 182,000 survivors of the dis- aster; another $3.2 billion was provided to state and local governments for debris removal, infrastructure repair, and emergency protective measures. More than $2.4 billion was provided to individuals and businesses in the form of low-interest loans through the Small Business Administration (“SBA”), and millions more were spent on grants de- signed to implement mitigation measures in the future and to provide unemployment assistance to survivors. Before the storm, homeowners paid premiums for flood insurance provided through the National Flood Insurance Program (“NFIP”), and for homeowner’s insurance provided by dozens of private insurers. In the months following the storm, they began to file claims for assistance in rebuilding their homes. While many such claims were re- solved successfully, many homeowners were unhappy with the settlement amounts offered by their insurance carriers and felt compelled to file lawsuits in the surrounding state and federal courts. Many of those lawsuits were filed in the United States District Court for the Eastern District of New York (“EDNY”). This case study describes the EDNY’s specifically crafted, unique approach to handling the mass litigation that ensued from Sandy’s devastation, documents some of the problems that the Court faced during that mass litigation, and describes some of the lessons learned from the Court’s experience.

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15

Newton, Alicia. "Sandy storehouse". Nature Climate Change 1, n.º 805 (17 de abril de 2008): 50. http://dx.doi.org/10.1038/climate.2008.34.

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16

Lindsey, Heather. "Hurricane Sandy". Nephrology Times 5, n.º 12 (diciembre de 2012): 8–11. http://dx.doi.org/10.1097/01.nep.0000426009.16085.b8.

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17

Healy, Sonya y Gundersen Lutheran. "Sandy Littlejohn". Nurse Leader 4, n.º 3 (junio de 2006): 10–13. http://dx.doi.org/10.1016/j.mnl.2006.04.001.

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18

Hewitt, Paul. "SANDY BOTTOM". Physics Teacher 46, n.º 8 (noviembre de 2008): 454. http://dx.doi.org/10.1119/1.2999058.

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19

Trento, Laura y Sarah Allen. "Hurricane Sandy". Nutrition in Clinical Practice 29, n.º 5 (25 de junio de 2014): 576–84. http://dx.doi.org/10.1177/0884533614536927.

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20

Richter, Matt. "Occupy Sandy". Disaster Medicine and Public Health Preparedness 6, n.º 4 (diciembre de 2012): 324. http://dx.doi.org/10.1001/dmp.2012.75.

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21

Chmiel, Stanisław, Stanisław Hałas, Sławomir Głowacki, Joanna Sposób, Ewa Maciejewska y Andrzej Trembaczowski. "Concentration of soil CO2 as an indicator of the decalcification rate after liming treatment". International Agrophysics 30, n.º 2 (1 de abril de 2016): 143–50. http://dx.doi.org/10.1515/intag-2015-0085.

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Abstract This paper presents the results of investigation of decalcification of acid sandy and loamy sand soils by infiltration waters, and potential Ca-leaching after liming treatment. For this purpose, monthly measurements were made of the concentration of CO2 in the soil air, dissolved inorganic carbon in the soil waters, and their ionic composition. The determined dissolved inorganic carbon ranged from 5.9 to 10.6 mg dm−3 and from 9.9 to 16.5 mg dm−3 for the sandy and loamy sand soil, respectively. The Ca concentration in soil waters was determined as 5.9-12.4 mg dm−3 in sandy soil and 14.2-19.8 mg dm−3 in soil loamy sand. The calculated rate of decalcification amounted to 23.0 kg ha−1 year−1 in soil sandy and 19.4 kg ha−1 year−1 in loamy sand soil. The potential Ca-leaching is predicted as 124 kg ha−1 year−1 for S and 87 kg ha−1 year−1 for loamy sand soil. At the treatment level of 3 000 kg ha−1 4 year−1 of CaO, ~20% of the Ca-fertilizer can be leached after the liming treatment. The results of the CO2 concentration in the soil air may be useful in estimation of Ca-leaching from soils developed by slightly clayey sands and clayey sands in zones with a moderate climate.

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22

Lange, Ivan, Pavel Kotiukov y Yana Lebedeva. "Analyzing Physical-Mechanical and Hydrophysical Properties of Sandy Soils Exposed to Long-Term Hydrocarbon Contamination". Sustainability 15, n.º 4 (15 de febrero de 2023): 3599. http://dx.doi.org/10.3390/su15043599.

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This paper aims to investigate the issue of sandy soil contamination by oil hydrocarbons. Laboratory procedures used to study conditionally pure and contaminated sands include grain-size measurements and evaluation of physical-mechanical and hydrophysical properties. The results of the analysis of sand samples using visual and microscopic studies and sieve analysis show that, unlike in conditionally pure sands, in contaminated samples, the surface of mineral particles is covered by hydrocarbon film. The presence of the latter enables micro- and macroaggregates to be formed. Studies of the physical and hydrophysical properties of sands using a technique with pre-weighed glass containers, as well as a filtering device, SPETSGEO pipes, showed that, in comparison with conditionally pure samples, contaminated specimens of sandy soils have lower densities and higher permeabilities and water yields. Testing the mechanical properties of contaminated sands on the GPP-30 direct shear apparatus using the consolidated dried shear strength method revealed an increase in the angle of internal friction with a decrease in specific adhesion compared to conditionally clean sands.

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23

Yatsyshyn, Andriy, Maciej Bąbe, Danuta Olszewska-Nejber, Andriy Bogucki y Stephania Vas’kiv. "Lithological and sedimentological characteristics of the alluvium of the sixth terrace of the Dniester river (Loyeva level) in the Torhanovychi 2 section". Visnyk of the Lviv University. Series Geography, n.º 41 (17 de septiembre de 2013): 382–95. http://dx.doi.org/10.30970/vgg.2013.41.2011.

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The main lithological characteristics of the alluvium of the sandy-gravelly bed of the sixth terrace of the Dniester river (Loyeva level) at environs of Sambir was analysed, in particular textural elements, granulometric and petrographic composition of the gravelly material (enclosing coarse sands, granules, pebbles, cobbles and boulders), its roundness, and the orientation of grains. The conditions of sedimentation of the studied alluvial sandy-gravelly bed of the sixth terrace of the Dniester river (Loyeva level) were reconstructed. Key words: granulometric composition, petrographic composition, roundness, sorting, imbrication, braided channel, depositional conditions.

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24

Łabuz, Tomasz Arkadiusz, Ralf Grunewald, Valentina Bobykina, Boris Chubarenko, Algimantas Česnulevičius, Artūras Bautrėnas, Regina Morkūnaitė y Hannes Tõnisson. "Coastal Dunes of the Baltic Sea Shores: A Review". Quaestiones Geographicae 37, n.º 1 (30 de marzo de 2018): 47–71. http://dx.doi.org/10.2478/quageo-2018-0005.

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Abstract The article summarises results of studies conducted along the Baltic Sea sandy coasts by scientists involved in coastal dune research, and presents an attempt to describe the types and distribution of dune coasts. The Baltic Sea coasts feature lower and higher foredunes. The lowland behind the coastal dune belt is covered by wandering or stabilised inland dunes – transgressive forms, mainly parabolic or barchans. The source of sediment for dune development includes fluvioglacial sands from eroded coasts, river-discharged sand, and older eroded dunes. Due to the ongoing erosion and coastal retreat, many dunes have been eroded, and some are withdrawing onto the adjacent land. There are visible differences between the south-eastern, western, and northern parts of the Baltic Sea coast with respect to dune development. The entire southern and eastern coast abounds in sand, so the coastal dunes are large, formerly or currently wandering formations. The only shifting dunes are found at the Polish and the Russian–Lithuanian coasts on the Łebsko Lake Sandbar as well as on the Vistula and Curonian Spits. The very diverse shoreline of the south-western coast experiences a scarcity of larger sandy formations. Substantial parts of the Baltic Sea sandy coasts have been eroded or transformed by humans. The northern part of the Baltic Sea coast features mainly narrow and low sandy coasts (e.g. in Estonia). Further north, sandy dunes are virtually absent.

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25

Stanila, Anca Luiza, Catalin Cristian Simota, Iulian Ratoi, Aurelia Diaconu y Mihail Dumitru. "Research on Improving Fertility Sandy Soils from Dabuleni Field by Administration of Loess". Revista de Chimie 70, n.º 2 (15 de marzo de 2019): 543–48. http://dx.doi.org/10.37358/rc.19.2.6952.

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In order to solve and clarifying certain aspects of the clay content (particles [0.002 mm) sands and sandy soils, humus, respectively, the process of bioaccumulation and mineralization the organic matter of the land, in the Research and Development Centre for Plant Growing on Sand Dabuleni, have initiated research aimed at finding methods and means for accumulating and thus the increase in the content of clay in the soil, respectively humus.Therefore, to improve radical of sandy soils, we found it necessary to resort to what is called loess process. It consists in enriching the horizon the surface soil (20-25 cm) the fraction with 8-10% clay, to 1.5-5%, as currently it contains. It is primarily intended to influence various amounts loess material on physical, hydro- physical and chemical properties of soils, then the plant response to changes products in the soil, increasing the guaranteed potential fertility of these soils, which will result in production high and constant.Obtaining appropriate agricultural production on sandy soils (eutric psamosol) it is limited not only by the soil, but also other factors such as relief, drainage and even climate. Because coarse texture, water-holding capacity in the case of sandy soils it is very low in all soils, the clay content below 5% production capacity of soils it is particularly low in the absence of agropedoameliorative measures and especially irrigation. Wind erosion occurs in all perimeters sandy soils, with higher intensity is observed in Oltenia Plain (Dabuleni Field).

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26

Guan, Chengli y Yuyou Yang. "Field Study on the Waterstop of the Rodin Jet Pile Method in a Water-Rich Sandy Gravel Stratum". Applied Sciences 9, n.º 8 (25 de abril de 2019): 1709. http://dx.doi.org/10.3390/app9081709.

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Due to the increasing depths of underground urban construction, the surrounding environment and hydrogeological conditions are becoming increasingly complex, and conventional high-pressure rotary jet grouting has become unable to meet construction needs. At present, Rodin jet pile (RJP) ultra-high-pressure rotary jet grouting has been widely used as a grouting reinforcement method for deep and large foundations in silty soils, fine sands and clay strata; however, there have been no successful applications in a sandy gravel stratum with high water content (namely, water-rich sandy gravel stratum). Therefore, this paper uses the ventilating shaft in a section of the Beijing Metro as the construction background to carry out field tests on the RJP ultra-high-pressure rotary jet grouting method and waterstop in a water-rich sandy gravel stratum. Through a series of experiments monitoring the formation deformation and pore water pressure and exposing the pile diameter, pile occlusion, pile strength, and permeability of the test pile construction process, it is believed that, for the RJP ultra-high-pressure construction method in a water-rich sandy gravel stratum, reliable jet solidification can occur, the joint between jets can be achieved, the solid strength can reach 10 MPa or higher, and the permeability coefficient can reach 10−8 cm/s. Therefore, RJP ultra-high-pressure rotary jet grouting can be applied as a waterstop method in water-rich sandy gravel stratum.

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27

Cauxeiro, Cirilo, Michel Lopez, Javier Hernández-Molina, Artur Miguel, Gizela Cauxeiro y Vanessa Caetano. "Contourite vs Turbidite Outcrop and Seismic Architectures". Angolan Mineral, Oil & Gas Journal 1, n.º 1 (6 de mayo de 2020): 20–26. http://dx.doi.org/10.47444/amogj.v1i1.9.

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The hydrocarbon exploration of oceanic depositional systems demands a better understanding of the role of bottom currents and their implications for petroleum systems such as reservoir and sealing rocks. Deep-marine bottom-current reworked sands (sandy contourites) have been recognized in hydrocarbon-bearing sands of the Kwanza Basin. Such understanding implies additional alternatives for the definition of exploration targets and prospect risk reduction. The southernmost part of the Kwanza Basin (Miradouro da Lua zone) comprises one of the best outcrops of contourites deposits, formed during the Miocene and Pliocene age. Laterally, coeval sandy deposits are found offshore Kwanza Basin along the continental margin, and have been one of the great challenges for the oil companies operating in Angola. Therefore, the aim of the current proposal is to characterize sandy contourite deposits at Miradouro da Lua and compare them with offshore deep-water sandy deposits, evaluating their conceptual and economic implication. Modern field sedimentology technique merged with reflection seismic data and other geographic information system (GIS) techniques, allow the characterization and proposal of a stratigraphic architecture diagram that explains the interaction of the deep-marine processes, especially gravitational (down-slope) and bottom current (along-slope) processes as well as its vertical and spatial association. Sonangol (Angolan State Oil Company) and Total (French Multinational Company) explore similar deposits in Block 48 in Ultra deep-sea, and they will also reactivate the exploration of the Iabe Formation in Block 4. The Tertiary Stratigraphic Architecture in Blocks 6, 7, 8, 19 and 20 are similar to the Lower part of the Miradouro da Lua zone. All these observations and data are very important to calibrate oil reservoir models.

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28

Aziz, Mike y Alexis Georges. "Aménager après Sandy". Outre-Terre 35-36, n.º 1 (2013): 483. http://dx.doi.org/10.3917/oute.035.0483.

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29

Urquhart, Steve. "Sandy Ross Urquhart". Veterinary Record 188, n.º 5 (marzo de 2021): 196. http://dx.doi.org/10.1002/vetr.282.

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30

Neal, Ryann y Robert Fischer. "Weathering SuperStorm Sandy". Proceedings of the Water Environment Federation 2014, n.º 17 (1 de octubre de 2014): 2320–38. http://dx.doi.org/10.2175/193864714815943557.

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31

Roulstone, Ian y John Norbury. "Computing Superstorm Sandy". Scientific American 309, n.º 2 (17 de julio de 2013): 22. http://dx.doi.org/10.1038/scientificamerican0813-22.

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32

Ersel, Murat. "Aftermath Hurricane Sandy". Journal of Academic Emergency Medicine 12, n.º 2 (24 de mayo de 2013): 110–11. http://dx.doi.org/10.5152/jaem.2013.032.

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33

Chambers, G. "Alexander 'Sandy' Smith". International Journal of Dairy Technology 55, n.º 4 (noviembre de 2002): 217–18. http://dx.doi.org/10.1046/j.1471-0307.2002.00074.x.

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34

Hutner, H. "Hurricane Sandy Diary". Interdisciplinary Studies in Literature and Environment 21, n.º 1 (19 de marzo de 2014): 59–67. http://dx.doi.org/10.1093/isle/isu019.

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35

Hardy, R. "Sandy Holt-Wilson". BMJ 349, jul25 7 (25 de julio de 2014): g4846. http://dx.doi.org/10.1136/bmj.g4846.

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36

Weeks, C. "Sandy (Alexander) Pinkerton". Spinal Cord 49, n.º 3 (marzo de 2011): 322. http://dx.doi.org/10.1038/sc.2010.135.

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37

Malekoff, Andrew. "Sandy and Sandy in Seven Weeks: A Group Worker Reflects". Social Work With Groups 36, n.º 4 (octubre de 2013): 285–91. http://dx.doi.org/10.1080/01609513.2013.796543.

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38

Sun, Lei, Yuanyun Xie, Chunguo Kang, Yunping Chi, Peng Wu, Zhenyu Wei, Siqi Li, Qian Zhao y Shuo Liu. "The composition of heavy minerals of the sandy lands, Northeast China and their implications for tracing detrital sources". PLOS ONE 17, n.º 10 (20 de octubre de 2022): e0276494. http://dx.doi.org/10.1371/journal.pone.0276494.

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Comprehending heavy mineral composition of the sandy land in Northeast China (NESL) is of great significance for interpreting generation, pathways, source and geochemistry of sediments in this area. To this end, the fine-grained (<63 μm) aeolian-fluvial sediments and loess deposits, which were taken from the Onqin Daga Sandy Land, the Horqin Sandy Land, the Hulun Buir Sandy Land and the Songnen Sandy Land, and from the downwind loess section (L1), respectively, were analyzed to construct the heavy mineral data set of NESL source and sink and to evaluate feasibility of the heavy mineral method in tracing the source of aeolian dust in Northeast China. Additionally, the <63 μm, 63–125 μm and 125–250 μm fractions of the fluvial sands from the different Balan River reaches having a same source, were analyzed to valuate the impact of the river transport-sedimentation process on the heavy mineral composition. The results show that the NESL shows moderate similarities in the heavy mineral composition, with ilmenite, epidote, zircon and amphibole as the primary minerals. In the source-to-sink system in the NESL, limited by sedimentary differentiation, post-deposition alteration and similar source material composition, the heavy mineral composition of the loess and that of sandy-land sources does not well correlate, indicating single heavy mineral method is incapable of unequivocally detecting loess sources when not considering the physical geographical conditions. The sediments in the different Balan River reaches show clear diversities and grain-size dependency in heavy minerals composition, indicating the river transport-deposition processes exert a clear control on the heavy-mineral composition in the sediment downstream. Both a wide grain-size window and more numbers of samples are needed to obtain a complete heavy-mineral picture in the source area.

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39

Caputa, Zbigniew. "The structure of the radiation balance on a sandy surface: case the Błędów desert, Silesian Upland". Ekológia (Bratislava) 35, n.º 2 (1 de junio de 2016): 114–25. http://dx.doi.org/10.1515/eko-2016-0009.

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AbstractComprehensive environmental studies taking under consideration the structure of the radiation balance during the vegetation growing seasons of 2001 and 2002 were carried out on the open sandy surface of the area called the Błędów ‘desert’ located on Silesian Upland. The research in each site covered the composition of plant species, their age and height, the condition of the substratum, the composition and structure of the soil and the meteorological conditions with elements of the radiation balance. The article presents some part of the research on meteorological elements and their impact on ecosystem. Special attention was devoted to radiation conditions on the open sandy surface in the context of the formation of BSC (biological soil crust). Having presumed that the values obtained on the grassy surface constituted 100%, the values of radiation reflection measured on the open sandy surface were 185% higher and the values of net longwave radiation were 105% higher in day time and 137% in night time. Values of net radiation of about 63% lower were observed on the sandy surface during a typical sunny summer day. It was found that a strong irradiation of the sandy surface (26 MJ·m–2d–1) creates extremely difficult conditions for the initiation of the process of ecosystem formation (including BSC or plant succession). The elements of the radiation balance, net radiation, albedo and temperature of the open sandy surface were represented quantitatively. The test surfaces were classified based on the value of the albedo: group I with low albedo values, up to 0.15 (spore-bearing plants on a dark surface), including BSC; group II with mean values of the albedo from 0.16 to 0.24 (spore-bearing plants and seed on a dark grey surface); and group III with high albedo values, above 0.25 (plants growing on bare or loose sands).

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40

RYASHCHENKO, TAMARA y STANISLAV MAKAROV. "Mineral composition of eluvial and aeolian sands (on the example of the unique collection of samples)". Domestic geology, n.º 5 (15 de noviembre de 2022): 59–69. http://dx.doi.org/10.47765/0869-7175-2022-10030.

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The object of the research is the unique collection of samples of eluvial and aeolian sands collected in the tropical (Vietnam) zone and the zone with the temperate humid sharply continental climate (the Tunkinsk’s depression in the Baikal region). Traces of structural connectivity were established by visual inspection of the samples in laboratory conditions using a four-fold magnifier. "Cohesive" clayey (ps*) and ordinary sandy (ps) varieties were identified. The mineral composition of the collection sands was determined by the method of quantitative immersion analysis of the 0.25–0.05 mm fraction. The composition and morphological characteristics of various light and heavy terrigenous minerals were determined, and special coefficients were calculated using the method of quantitative immersion analysis. Beforehand, the granulometric analysis of samples was carried out using A.N. Sabanin's method. As a result, the fraction for mineralogical studies was isolated, and the content of sandy-pulverescent and clay particles was established. The research goal consists of a comparative analysis of the mineral composition of the sands, the degree of their chemical maturity, and the investigation of possible variants of structural connectivity formation.

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41

Xu, Yan, Zhaoyang Cai, Kaige Wang, Yuwei Zhang y Fengrong Zhang. "Evaluation for Appropriate Tillage of Sandy Land in Arid Sandy Area Based on Limitation Factor Exclusion Method". Land 11, n.º 6 (30 de mayo de 2022): 807. http://dx.doi.org/10.3390/land11060807.

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Investigating and evaluating the quantity and spatial distribution of arable sandy land in arid and semiarid sandy areas is of great significance for the sustainable development and utilization of sandy land resources and the maintenance of the stability of the structure and function of regional ecosystems. Based on the characteristics of sandy soil, being without structure and susceptible to wind erosion, this study used the limiting factor exclusion method to investigate and evaluate arable sandy land in arid and semiarid areas. All sandy soils were taken as the evaluation objects of arable sandy land (including visible sandy land and invisible sandy land). On the basis of following the principle of ecological protection, the evaluation indicators and limiting factor exclusion evaluation methods of arable sandy land were determined. The results of Hangjin Banner are as follows: the total area of the visible sandy land and the recessive sandy land was 1.2 × 106 hm2; the visible sandy land accounted for 42.6%, and the invisible sandy land accounted for 57.5%. However, only 7.7% of the sandy land was suitable for farming, which is the current cultivated land of bare sand and sandy soil, extremely-low-coverage grassland, inland tidal flats, and other saline-alkali land. Even if these arable sandy lands are to be used sustainably after reclamation, reasonable ecological protection, irrigation engineering measures, and field protective farming measures must be taken. It is hoped that this study can provide a valuable reference for the sustainable development and utilization of arable sandy land and desertification control in arid and semiarid areas.

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42

Sivapalan, S. "Benefits of treating a sandy soil with a crosslinked-type polyacrylamide". Australian Journal of Experimental Agriculture 46, n.º 4 (2006): 579. http://dx.doi.org/10.1071/ea04026.

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The productivity of sandy soils is mostly limited by their low water-holding capacity and excessive deep percolation losses, which reduce the efficiency of water and fertiliser use by plants. The effect of a crosslinked-type polyacrylamide, ALCOSORB 400, on water-holding capacity of a sandy soil, siliceous sands, was studied under the laboratory and glasshouse conditions. Water-holding capacity of the soil exposed to 0.01 MPa increased by 23 and 95% by adding 0.03 and 0.07% of polyacrylamide to the soil, respectively. This indicated that the soil treated with polyacrylamide was able to store more water than untreated soil, thereby reducing the potential losses due to deep percolation in sandy soils. However, the polyacrylamide in the treated soil did not significantly increase the quantity of water released from the soil by increasing the pressure from 0.01 to 1.5 MPa. The results from the first glasshouse experiment demonstrated that the excess amount of water stored in the soil by polyacrylamide was available to plants and resulted in higher water use and grain production. Consequently, there was a 12 and 18 fold increase in water use efficiency of soybean plants grown in soils treated with 0.03 and 0.07% polyacrylamide, respectively. The results from the second glasshouse experiment demonstrated that increasing amounts of polyacrylamides in a sandy soil can extend the irrigation interval without any adverse effect on the grain yield of soybeans.

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43

Vyrkin, V. B. y D. V. Kobylkin. "Features of aeolian relief formation of the sandy massif Suvinskii Kuitun in the Barguzin Depression". IOP Conference Series: Earth and Environmental Science 885, n.º 1 (1 de octubre de 2021): 012041. http://dx.doi.org/10.1088/1755-1315/885/1/012041.

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Abstract The principal objective of the article is the determination of the main features of the aeolian relief formation of the Suvinskii Kuitun sand massif, one of the regions of active modern aeolian morphogenesis in the Barguzinskaya Depression. A brief description of the morphology of the aeolian relief, characterized by the predominance of deflationary forms over accumulative ones, is given. Among the forms of active deflation, deflation basins dominate here, separated by elongated deflation inselbergs, composed of sands of lacustrine, alluvial, deluvial-proluvial, and aeolian genesis. The mineralogical and granulometric composition of sandy deposits in the southern part of the Suvinskii Kuitun, characterized by poor roundness of sandy grains, has been analysed. A distinct northeastward eolomotion was revealed towards the foothills of the Ikat Range and its accumulation there. The age of the aeolian sands, mainly related to the formation of the Tagar culture (the end of the Bronze Age) was determined. The phytomelioration carried out in the second half of the 20th century led only to a partial fixation of sands, without affecting their overall deflation in most areas of the Suvinskii Kuitun.

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44

Lapietra, Isabella, Stefania Lisco, Luigi Capozzoli, Francesco De Giosa, Giuseppe Mastronuzzi, Daniela Mele, Salvatore Milli et al. "A Potential Beach Monitoring Based on Integrated Methods". Journal of Marine Science and Engineering 10, n.º 12 (8 de diciembre de 2022): 1949. http://dx.doi.org/10.3390/jmse10121949.

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This study focuses on the analysis of sandy beaches by integrating sedimentological, geomorphological, and geophysical investigations. The beach represents an extremely variable environment where different natural processes act simultaneously with human activities, leading to the gathering of different methodologies of the Earth Sciences to study its evolution in space and time. The aim of this research is to propose a potential procedure for monitoring the morpho-sedimentary processes of sandy beaches by analyzing the textural and compositional characteristics of the sands and quantifying the volumes involved in the coastal dynamics. The study area includes two Apulian sandy beaches (Torre Guaceto and Le Dune beach) that are representative of the coastal dynamics of a large sector of the central/northern Mediterranean Sea involving the southern Adriatic Sea and the northern Ionian Sea. Sedimentological and ecological investigations allowed to describe the textural and compositional characteristics of the beach sands by interpreting their sand provenance and the physical/biological interactions within the beach. The topographic surveys carried out with a Terrestrial Laser Scanner and an Optical Total Station, aimed to quantify the variations of sediment volume over time, whereas the Delft3d software was applied to analyze the effects of the dominant wave motion on the sedimentary dynamics. Lastly, the geophysical techniques which included Sub Bottom Profiler procedures, Ground Penetrating Radar investigation, and resistivity models enabled us to calculate the sand sediment thickness above the bedrock.

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45

Daniels, W. L., M. H. Genthner y R. L. Hodges. "Soil Development in Sandy Tailings Derived from Mineral Sands Mining in Florida". Journal American Society of Mining and Reclamation 1992, n.º 1 (1992): 37–47. http://dx.doi.org/10.21000/jasmr92010037.

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46

Yair, A. "Runoff generation in a sandy area—the nizzana sands, Western Negev, Israel". Earth Surface Processes and Landforms 15, n.º 7 (noviembre de 1990): 597–609. http://dx.doi.org/10.1002/esp.3290150703.

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47

Fibrianty, A. Ma’as, E. Hanudin y P. Sudira. "Improvement The Fertility of Sandy Soil Amended using Bagasse and Different Type of Soil to The Yield of Shallot". IOP Conference Series: Earth and Environmental Science 985, n.º 1 (1 de febrero de 2022): 012056. http://dx.doi.org/10.1088/1755-1315/985/1/012056.

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Abstract The sandy soil in Samas Beach, Yogyakarta is characterized by the dominance of sand fraction, high leaching of nutrient, and high soil temperature. Shallot cultivation is possible in coastal sandy land through modification of microclimate and improvement of soil fertility. This study aimed to determine the effect of improving physical and chemical fertility of sandy soil amended by clay soil and bagasse to the yield of shallot. The study was conducted using Randomized Block Design with four treatments and four replications: Sandy Soil (S), Sandy soil + Bagasse (SB), Sandy soil + Latosol + Bagasse (SLB), Sandy Soil + Grumusol + Bagasse (SGB). Amendment increased moisture contents and decreased the permeability of sandy soil. SGB improved the highest water holding capacity, organic C and Total N of sandy soil. The highest yield of shallot reached at application of SLB and SGB, these treatments produced total dry weight of shallot, which were 19.63 and 23.85 g clump-1. The combination of clay soil and bagasse was recommended as the amendment technology to improve the fertility of sandy soil.

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48

Stanila, Anca-Luiza, Iulian Ratoi, Aurelia Diaconu y Catalin Cristian Simota. "The Results Obtained on Production of Alfalfa on Sandy Soils of Field Dabuleni by Administration of Loess and Chemical Fertilizers". Revista de Chimie 71, n.º 2 (3 de marzo de 2020): 30–34. http://dx.doi.org/10.37358/rc.20.2.7887.

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Recovery sandy soils top was a major concern, sandy soil cultivation with the crop plants had the main goal need to increase the agricultural production. Sands in southern Oltenia offers less favorable conditions of plant life, which is why the range of cultivated plants is much lower than in other areas.Seed plants that require small and early seed (alfalfa) are affected by the negative effect of the wind, which blows away the sand particles, lesion rooted young plants or compromising their culture. On sandy soils in southern Oltenia (Field Dabuleni), forage crops help to improve physical, hydro-chemical properties, change the living conditions for plants, animals and humans, create an ecological balance that preserves the environment, partly destroyed by abolishing plantations of Robinia pseudocacia and leveling dunes relief for arranging irrigation.Among perennial leguminous pure culture, alfalfa is the most valuable forage plant feed all animal species, both for its output, especially for forage quality. Achieving quality parameters alfalfa is conditional, namely the establishment of the following technologies, namely: mowing standing of the optimal phenological stages of the plant, the establishment range of mowing or the number of harvest in a year.

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49

Ritz, Sandy y Marietta Lee. "AJN Interview: Sandy Ritz". American Journal of Nursing 95, n.º 8 (agosto de 1995): 39. http://dx.doi.org/10.2307/3471136.

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50

Reeves, D. L. y L. Hall. "Registration of ‘Sandy’ Oat". Crop Science 40, n.º 4 (julio de 2000): 1191–92. http://dx.doi.org/10.2135/cropsci2000.0034rcv.

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