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Journal articles on the topic 'Soil and Water Sciences'

Author: Grafiati

Published: 4 June 2021

Last updated: 20 February 2023

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1

Raats, P. A. C. "Applications of material coordinates in the soil and plant sciences." Netherlands Journal of Agricultural Science 35, no. 3 (August 1, 1987): 361–70. http://dx.doi.org/10.18174/njas.v35i3.16731.

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The continuum theory of mixtures is used to show the common basis of models in three areas. In each, the central problem is the description of the deformation and motion of a reference continuum and of the movement of one or more constituents relative to this reference continuum. The three applications concern the movement of solutes relative to soil water, the movement of soil water relative to the solid phase of swelling/shrinking soils, and the movement of water, solutes, and gases relative to growing plant tissues. (Abstract retrieved from CAB Abstracts by CABI’s permission)

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2

Thomas, R. L. "Soil and water science." Soil and Tillage Research 42, no. 1-2 (May 1997): 141–42. http://dx.doi.org/10.1016/s0167-1987(97)83358-2.

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3

Kroulík, M., J. Hůla, R. Šindelář, and F. Illek. "Water infiltration into soil related to the soil tillage intensity." Soil and Water Research 2, No. 1 (January 7, 2008): 15–24. http://dx.doi.org/10.17221/2098-swr.

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Soil infiltration capacity is one of the key factors in the soil protection against unfavourable effects of water erosion. The purpose of its measuring was to compare and evaluate the changes of the soil physical properties and of water infiltration into soil caused by different intensity of soil cultivation at two individual sites. The ploughing (PL), shallow tillage (ST), and direct drilling (NT) effects on the soil physical properties, water infiltration into soil, and soil surface coverage with the crop residua under the soil condition loamy Haplic Luvisol, with long-term growing of maize

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4

Ende, J. van den. "Water contents of glasshouse soils at field capacity and at saturation. 1. Relationships between water contents." Netherlands Journal of Agricultural Science 36, no. 3 (August 1, 1988): 265–74. http://dx.doi.org/10.18174/njas.v36i3.16678.

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The relationship between water contents at saturation and at field capacity was determined in soils from 75 glasshouses in the Netherlands. Sandy, loamy and peaty soils were equally represented. Water contents of soils at sampling time were found to correspond closely with those at field capacity. Water contents of saturated pastes obtained from field-moist soil samples were higher than those of saturated pastes obtained from soil samples dried previously. For the relationships between water contents of field-moist soil samples and of saturated pastes obtained from field-moist and dried soil s

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5

Bouma, Johan. "Soil Security in Sustainable Development." Soil Systems 3, no. 1 (January 8, 2019): 5. http://dx.doi.org/10.3390/soilsystems3010005.

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The United Nations (UN) Sustainable Development Goals (SDGs) provide an excellent channel to demonstrate the significance of soils when considering e.g., food production, water availability, climate mitigation and biodiversity preservation. For environmental sciences, including soil science, the SDGs provide “a point at the horizon” for future research. Progress to achieve the SDGs by 2030 will bureaucratically be monitored by targets and indicators but questions as to how effective research should be organized remain unanswered so far. The soil security concept, based on the five Cs (capabili

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6

Brillante, L., O. Mathieu, B. Bois, C. van Leeuwen, and J. Lévêque. "The use of soil electrical resistivity to monitor plant and soil water relationships in vineyards." SOIL 1, no. 1 (March 17, 2015): 273–86. http://dx.doi.org/10.5194/soil-1-273-2015.

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Abstract. Soil water availability deeply affects plant physiology. In viticulture it is considered a major contributor to the "terroir" effect. The assessment of soil water in field conditions is a difficult task, especially over large surfaces. New techniques are therefore required in order to better explore variations of soil water content in space and time with low disturbance and with great precision. Electrical resistivity tomography (ERT) meets these requirements for applications in plant sciences, agriculture and ecology. In this paper, possible techniques to develop models that allow t

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7

Pierzgalski, Edward, and Jerzy Jeznach. "Measures for soil water control in Poland." Journal of Water and Land Development 10, no. 1 (December 1, 2006): 79–89. http://dx.doi.org/10.2478/v10025-007-0007-5.

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Measures for soil water control in Poland Polish water resources depend on precipitations, which are variable in time and space. In dry years the water balance is negative in central parts of Poland but sudden thaws and downfalls may result in periodical water excess and dangerous floods almost in the entire country. The retention capacity of artificial reservoirs in Poland permits to store only 6% of the average annual runoff, which is commonly considered insufficient. Another method to increase retention is soil water control. About fifty percent of soils in Poland consist of light and very

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8

Judy, Jonathan D., Maria L. Silveira, Sampson Agyin-Birikorang, George O'Connor, and Thomas A. Obreza. "Drinking Water Treatment Residuals to Control Phosphorus in Soils." EDIS 2019 (August 21, 2019): 6. http://dx.doi.org/10.32473/edis-ss513-2019.

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Soils in Florida may contain excess soil phosphorus (P) resulting from fertilizer, manure or biosolids applications. Excess P in soil does not damage soil fertility but can be transported from agricultural and urban areas either dissolved in water that drains away or as particulate matter (attached to soil particles) that travels with eroding soil. Increased P in water bodies is recognized as one of the major factors responsible for eutrophication-related decrease in water quality. Most soils have the capacity to retain excess P. However, soils with low capacity to retain excess P are abundant

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9

de Jonge, Lis W., Per Moldrup, and Ole H. Jacobsen. "SOIL-WATER CONTENT DEPENDENCY OF WATER REPELLENCY IN SOILS." Soil Science 172, no. 8 (August 2007): 577–88. http://dx.doi.org/10.1097/ss.0b013e318065c090.

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10

Wang, Xiaofang, Yi Li, Yichen Wang, and Chuncheng Liu. "Performance of HYDRUS-1D for simulating water movement in water-repellent soils." Canadian Journal of Soil Science 98, no. 3 (September 1, 2018): 407–20. http://dx.doi.org/10.1139/cjss-2017-0116.

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Soil water repellency affects soil water movement during infiltration significantly. The HYDRUS software has been popularly applied in soil water dynamics simulation for many years, but its performance in water-repellent (WR) soils has not been assessed thoroughly. Our objectives are to assess the performance of HYDRYUS-1D for cumulative infiltration (CI), wetting front (Zf), and volumetric soil water content (θv) during horizontal imbibition and vertical infiltration in wettable, slightly WR, and strongly WR soils. The key parameters of α and n in water retention curves were inversely estimat

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11

Kolmogorov, S. G., P. L. Klemyatsionok, and S. S. Kolmogorova. "Toward compaction of overmoistured clay soil." Vestnik Tomskogo gosudarstvennogo arkhitekturno-stroitel'nogo universiteta. JOURNAL of Construction and Architecture 24, no. 5 (October 27, 2022): 145–50. http://dx.doi.org/10.31675/1607-1859-2022-24-5-145-150.

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Various complicated processes, including physical and chemical, occur in clay soils, which finally determine their strength and stress-and-strain properties. In order to use clay soils as a subgrade, it is necessary to increase their strength primarily through a compaction. In clay soil compaction, the main role belongs to physically bound water, which gathers around soil particles forming water envelopes and making the compaction difficult. The paper considers compaction of overmoistured clay soils along with vibration, that provides an intensive transition of bound water to a free state. In

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12

Shober, Amy L., Alexander Joseph Reisinger, Mary G. Lusk, and Sally Ann Scalera. "Soils and Fertilizers for Master Gardeners: Soil Physical Characteristics." EDIS 2019, no. 4 (July 26, 2019): 7. http://dx.doi.org/10.32473/edis-mg458-2019.

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Soils are a foundational component of the landscape, providing a medium for plant root growth and playing a crucial role in nutrient cycling and water movement across the landscape. This new 7-page article describes the physical properties of soils, including soil formation in Florida, the soil profile, and water dynamics within soils, and provides a thorough reference for Master Gardeners and other individuals searching for a basic understanding of soil dynamics to apply to residential landscapes. Written by Amy L. Shober, Alexander J. Reisinger, Mary G. Lusk, and Sally Ann Scalera and publis

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13

Zhang, Hailin, Xiuyun Liu, Jun Yi, Xiufeng Yang, Tieniu Wu, Yi He, He Duan, Muxing Liu, and Pei Tian. "Bibliometric Analysis of Research on Soil Water from 1934 to 2019." Water 12, no. 6 (June 6, 2020): 1631. http://dx.doi.org/10.3390/w12061631.

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As an essential factor of the earth’s critical zone, soil water has a remarkable influence on nutrient cycle and energy flow in terrestrial ecosystems and has attracted the attention of considerable scholars. Based on the online database of Web of Science, the bibliometric analysis was performed to evaluate the evolution feature of soil water research from 1934 to 2019. The results showed a rapid growth of scientific outputs with a gradually increasing proportion of internationally collaborative articles. Environmental Sciences, Water Resources, and Soil Science were the most frequently used s

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14

Nielsen, Donald R., Miroslav Kutílek, and Marc B. Parlange. "Surface soil water content regimes: opportunities in soil science." Journal of Hydrology 184, no. 1-2 (October 1996): 35–55. http://dx.doi.org/10.1016/0022-1694(95)02967-2.

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15

Altobelli, Filiberto, Ronald Vargas, Giuseppe Corti, Carmelo Dazzi, Luca Montanarella, Alessandro Monteleone, Lucrezia Caon, et al. "Improving soil and water conservation and ecosystem services by sustainable soil management practices: From a global to an Italian soil partnership." Italian Journal of Agronomy 15, no. 4 (December 16, 2020): 293–98. http://dx.doi.org/10.4081/ija.2020.1765.

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The UN Sustainable Development Goals (SDGs) identify the need to restore degraded soils in order to improve productivity and the provision of ecosystem services. The aim is to support food production, store and supply clean water, conserve biodiversity, sequester carbon, and improve soil resilience in a context of climate change. Within this framework, in order to achieve the SDGs and to correct land management in the long-term, soil management is considered mandatory. The reduction of land degradation should be based on various sustainable soil management practices that improve and maintain s

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16

Dong, Yi, Changfu Wei, and Ning Lu. "Identifying Soil Adsorptive Water by Soil Water Density." Journal of Geotechnical and Geoenvironmental Engineering 146, no. 7 (July 2020): 02820001. http://dx.doi.org/10.1061/(asce)gt.1943-5606.0002289.

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17

Brillante, L., O. Mathieu, B. Bois, C. van Leeuwen, and J. Lévêque. "The use of soil electrical resistivity to monitor plant and soil water relationships in vineyards." SOIL Discussions 1, no. 1 (October 29, 2014): 677–707. http://dx.doi.org/10.5194/soild-1-677-2014.

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Abstract. Soil water availability deeply affects plant physiology. In viticulture it is considered as a major contributor to the "terroir" expression. The assessment of soil water in field conditions is a difficult task especially over large surfaces. New techniques, are therefore required to better explore variations of soil water content in space and time with low disturbance and with great precision. Electrical Resistivity Tomography (ERT) meets these requirements, for applications in plant sciences, agriculture and ecology. In this paper, possible techniques to develop models that allow th

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18

Hu, Jun, Xinbin Wang, Fujun Zhang, and Yuanke Zhao. "Experimental Study on the Variation of Soil Dielectric Permittivity under the Influence of Soil Compaction and Water Content." Geofluids 2022 (November 18, 2022): 1–9. http://dx.doi.org/10.1155/2022/3575541.

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The dielectric permittivity of common soils is mainly controlled by water content and porosity, while the latter is closely related to the characteristics of compaction. By studying the changes in dielectric permittivity of soil samples with different soil water content and compaction levels, the influence of the controlling factors on the relationship model between soil water content and dielectric permittivity can be evaluated. In this paper, network analyzer was used to measure the dielectric permittivity of 7 groups of soil samples with gravimetric water content ranging from 8.09% to 14.52

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19

Padarian, José, Budiman Minasny, and Alex B. McBratney. "Machine learning and soil sciences: a review aided by machine learning tools." SOIL 6, no. 1 (February 6, 2020): 35–52. http://dx.doi.org/10.5194/soil-6-35-2020.

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Abstract. The application of machine learning (ML) techniques in various fields of science has increased rapidly, especially in the last 10 years. The increasing availability of soil data that can be efficiently acquired remotely and proximally, and freely available open-source algorithms, have led to an accelerated adoption of ML techniques to analyse soil data. Given the large number of publications, it is an impossible task to manually review all papers on the application of ML in soil science without narrowing down a narrative of ML application in a specific research question. This paper a

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20

Yu, Dandan, Feilong Hu, Kun Zhang, Li Liu, and Danfeng Li. "Available water capacity and organic carbon storage profiles in soils developed from dark brown soil to boggy soil in Changbai Mountains, China." Soil and Water Research 16, No. 1 (December 11, 2020): 11–21. http://dx.doi.org/10.17221/150/2019-swr.

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The available water capacity (AWC) is the most commonly used parameter for quantifying the amount of soil water that is readily available to plants. Specific AWC and soil organic carbon storage (SOCS) profiles are consequences of the soil development process. Understanding the distributions of AWC and SOCS in soil profiles is crucial for modelling the coupling between carbon and water cycle processes, and for predicting the consequences of global change. In this study, we determined the variations in the AWC and SOCS from the surface to a depth of 100 cm in soils developed from dark brown soil

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21

Zhang, Panpan, and Jianglong Shen. "Effect of brackish water irrigation on the movement of water and salt in salinized soil." Open Geosciences 14, no. 1 (January 1, 2022): 404–13. http://dx.doi.org/10.1515/geo-2022-0367.

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Abstract In China, fresh water resources are scarce, while brackish water resources are abundant. Reasonable utilization of brackish water is one of the important measures to alleviate the contradiction of water shortage. In order to study the effect of brackish water irrigation on water and salt transport in saline-alkali soils, one-dimensional brackish water infiltration experiments of soil columns were conducted. The influence of brackish water with different salinities on water and salt transport in salinized soil was compared and analyzed. The results showed that under brackish water irri

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22

Dari, Biswanath, Vimala D. Nair, and Willie G. Harris. "Parameters for Site-Specific Soil Phosphorus Loss Modeling from Soil Test Data." EDIS 2017, no. 2 (May 9, 2017): 4. http://dx.doi.org/10.32473/edis-ss656-2017.

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This 4-page fact sheet is part of the Soil Phosphorus Storage Capacity (SPSC) for Phosphorus Risk Assessment and Management series. This series is intended for use by those who are interested in management practices and policies that minimize the risk of phosphorus loss from soils. Written by Biswanath Dari, Vimala D. Nair, and Willie G. Harris and published by the Department of Soil and Water Sciences, February 2017. SL442/SS656: Parameters for Site-Specific Soil Phosphorus Loss Modeling from Soil Test Data (ufl.edu)

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23

Kaishwa, S. J., E. M. Marwa, J. J. Msaky, and W. N. Mwakalasya. "Uranium natural levels in soil, rock and water: assessment of the quality of drinking water in Singida Urban District, Tanzania." Journal of Water and Health 16, no. 4 (April 30, 2018): 542–48. http://dx.doi.org/10.2166/wh.2018.254.

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Abstract An analytical study was carried out to determine the level of uranium in the soil and rock and associate it with the levels in surface and underground water, which are the main sources of drinking water in Singida Urban District, Tanzania. Fifteen water samples, 12 soil samples and nine rock samples were collected in Singida Urban District in February 2016. Water samples were analysed by the Government Chemist Laboratory Agency using inductively coupled plasma optical emission spectrometry (ICP-OES) (2007) and analyses for soil and rock samples were carried out through total X-ray flu

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Orfanus, Tomas, Abdel-Monem Mohamed Amer, Grzegorz Jozefaciuk, Emil Fulajtar, and Anežka Čelková. "Water vapour adsorption on water repellent sandy soils." Journal of Hydrology and Hydromechanics 65, no. 4 (December 20, 2017): 395–401. http://dx.doi.org/10.1515/johh-2017-0030.

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AbstractSoil sorptivity is considered a key parameter describing early stages of water (rain) infiltration into a relatively dry soil and it is related to build-up complexity of the capillary system and soil wettability (contact angles of soil pore walls). During the last decade an increasing water repellency of sandy soils under pine forest and grassland vegetation has been frequently observed at Mlaky II location in SW Slovakia. The dry seasons result in uneven wetting of soil and up to hundredfold decrease in soil sorptivity in these vegetated soil as compared to reference sandy material, w

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Ebel, B. A., E. S. Hinckley, and D. A. Martin. "Soil-water dynamics and unsaturated storage during snowmelt following wildfire." Hydrology and Earth System Sciences Discussions 9, no. 1 (January 11, 2012): 441–83. http://dx.doi.org/10.5194/hessd-9-441-2012.

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Abstract. Many forested watersheds with a substantial fraction of precipitation delivered as snow have the potential for landscape disturbance by wildfire. Little is known about the immediate effects of wildfire on snowmelt and near-surface hydrologic responses, including soil-water storage. Montane systems at the rain-snow transition have soil-water dynamics that are further complicated during the snowmelt period by strong aspect controls on snowmelt and soil thawing. Here we present data and analysis from field measurements of snow hydrology and subsurface hydrologic and temperature response

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26

Shevnin, V. A., D. I. Matveychuk, and A. S. Dernova. "Mapping of water resistivity using pool water." Moscow University Bulletin. Series 4. Geology, no. 5 (October 28, 2019): 81–83. http://dx.doi.org/10.33623/0579-9406-2019-5-81-83.

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In the papers of G.E. Archie and V.N. Dakhnov were presented formulas of dependence between resistivity (or conductivity) of soil and that of porous water. Such dependence shows that we need to know water resistivity, that means its study at each fieldwork area. In some areas places for groundwater are absent or restricted (boreholes, wells, springs) as places of surface water (rivers, streams, ponds, lakes). Can we measure water resistivity in pools? Immediately after rain such water has no relation with soil resistivity. The purpose of our study consists in determination the rules of ionic e

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27

Keesstra, Saskia, Srikanta Sannigrahi, Manuel López-Vicente, Manuel Pulido, Agata Novara, Saskia Visser, and Zahra Kalantari. "The role of soils in regulation and provision of blue and green water." Philosophical Transactions of the Royal Society B: Biological Sciences 376, no. 1834 (August 4, 2021): 20200175. http://dx.doi.org/10.1098/rstb.2020.0175.

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The United Nations Sustainable Development Goal 6 aims for clean water and sanitation for all by 2030, through eight subgoals dealing with four themes: (i) water quantity and availability, (ii) water quality, (iii) finding sustainable solutions and (iv) policy and governance. In this opinion paper, we assess how soils and associated land and water management can help achieve this goal, considering soils at two scales: local soil health and healthy landscapes. The merging of these two viewpoints shows the interlinked importance of the two scales. Soil health reflects the capacity of a soil to p

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28

Mundy, G. N., K. L. Greenwood, K. B. Kelly, S. M. Austin, and K. E. Dellow. "Improved soil and irrigation management for forage production 3. Plant - soil - water relationships." Australian Journal of Experimental Agriculture 46, no. 3 (2006): 327. http://dx.doi.org/10.1071/ea04097.

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A field experiment was conducted from January 2000 for 2.5 years, at the Department of Primary Industries, Kyabram, in northern Victoria. The experiment determined the effect of soil modification, with and without subsurface drainage, on the yield and water use of tall fescue (Festuca arundinacea), lucerne (Medicago sativa), phalaris (Phalaris aquatica) and perennial ryegrass (Lolium perenne) under 2 irrigation frequencies. The soil was a red-brown earth. The forages were spray irrigated from August to May when evaporation minus rainfall (E – R) reached 45–50 mm (frequent) or 90–100 mm (infreq

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Wraith, J. M. "Soil Water Dynamics." Vadose Zone Journal 3, no. 4 (November 1, 2004): 1490. http://dx.doi.org/10.2113/3.4.1490.

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Haverkamp, R., F. J. Leij, C. Fuentes, A. Sciortino, and P. J. Ross. "Soil Water Retention." Soil Science Society of America Journal 69, no. 6 (November 2005): 1881–90. http://dx.doi.org/10.2136/sssaj2004.0225.

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Leij, F. J., R. Haverkamp, C. Fuentes, F. Zatarain, and P. J. Ross. "Soil Water Retention." Soil Science Society of America Journal 69, no. 6 (November 2005): 1891–901. http://dx.doi.org/10.2136/sssaj2004.0226.

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Wraith, Jon M. "Soil Water Dynamics." Vadose Zone Journal 3, no. 4 (November 2004): 1490. http://dx.doi.org/10.2136/vzj2004.1490.

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GERMANN, PETER. "Soil- Water Interactions." Soil Science 146, no. 3 (September 1988): 210. http://dx.doi.org/10.1097/00010694-198809000-00014.

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Minasny, Budiman. "Soil Water Dynamics." Geoderma 122, no. 1 (September 2004): 103–4. http://dx.doi.org/10.1016/j.geoderma.2003.11.011.

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Su, Huidong, Yangwen Jia, Yongde Gan, Guangheng Ni, Cunwen Niu, Huan Liu, Tiantian Jin, and Yizhen Yao. "Soil water movement model for deformable soils." Journal of Water and Climate Change 11, no. 4 (July 22, 2019): 1191–202. http://dx.doi.org/10.2166/wcc.2019.262.

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Abstract To simulate the soil water movement process of deformable soils, a modified Richards model considering soil deformation (RMSD) was established. In the model, new parameters were introduced, including deformable soil porosity, deformable soil saturated hydraulic conductivity and unsaturated hydraulic conductivity of expansive soils, which varied with soil depth and time under the effect of soil deformation. The newly introduced parameters originated from physical properties of the soils and their calculation formulas were suggested. One-dimensional infiltration–runoff experiments were

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Bolland, MDA, and MJ Baker. "Increases in soil water content decrease the residual value of superphosphate." Australian Journal of Experimental Agriculture 27, no. 4 (1987): 571. http://dx.doi.org/10.1071/ea9870571.

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In pot experiments, levels of superphosphate incorporated through the whole soil were incubated for 30 days in 2 lateritic soils from south-western Australia at 1 of the following 5 soil water contents: air-dry for 30 days, at field capacity for 10 or 30 days, and flooded for 10 or 30 days. The soils were then air-dried for 30 days and the residual value of the superphosphate relative to freshly applied superphosphate was measured using 30-day-old triticale (x Triticosecale cv. Tyalla) and wheat (Triticum aestivum cv. Gamenya) plants. Soil samples were collected just before sowing from each po

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Michal, Dohnal, Dušek Jaromír, Vogel Tomáš, and Herza Jiří. "Analysis of Soil Water Response to Grass Transpiration." Soil and Water Research 1, No. 3 (January 7, 2013): 85–98. http://dx.doi.org/10.17221/6510-swr.

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This paper focuses on numerical modelling of soil water movement in response to the root water uptake that is driven by transpiration. The flow of water in a lysimeter, installed at a grass covered hillslope site in a small headwater catchment, is analysed by means of numerical simulation. The lysimeter system provides a well defined control volume with boundary fluxes measured and soil water pressure continuously monitored. The evapotranspiration intensity is estimated by the Penman-Monteith method and compared with the measured lysimeter soil water loss and the simulated root water uptake. V

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Mylavarapu, Rao, Willie Harris, and George Hochmuth. "Agricultural Soils of Florida." EDIS 2016, no. 9 (November 9, 2016): 7. http://dx.doi.org/10.32473/edis-ss655-2016.

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This 7-page fact sheet describes the various soil Orders in Florida, how they were developed, their characteristics, coverage in the state, and uses. This information is important for educating land owners, decision-makers, and educators about soils in Florida, leading to better soil management for agricultural and environmental sustainability. Written by Rao Mylavarapu, Willie Harris, and George Hochmuth, and published by the Soil and Water Sciences Department, October 2016. SL441/SS655: Agricultural Soils of Florida (ufl.edu)

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Chau, Henry Wai, Asim Biswas, Vladimir Vujanovic, and Bing Cheng Si. "Relationship between the severity, persistence of soil water repellency and the critical soil water content in water repellent soils." Geoderma 221-222 (June 2014): 113–20. http://dx.doi.org/10.1016/j.geoderma.2013.12.025.

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Hruska, K., and M. Kaevska. "Mycobacteria in water, soil, plants and air: a review." Veterinární Medicína 57, No. 12 (January 23, 2013): 623–79. http://dx.doi.org/10.17221/6558-vetmed.

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Amazingly, despite the 24 143 papers on mycobacteria, indexed in the Web of Science database during the last six years, published by 67 008 authors from 13 128 organizations located in 166 countries or territories, internationally accepted legal directives on how to control the public health risk associated with environmental mycobacteria have yet to be developed. Mycobacteria are human and animal pathogens, causing not only tuberculosis and leprosy, but mycobacterioses of skin, soft tissues and lung. Due to their cell wall composition and their adaptability mycobacteria can survive in differe

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Li, Shuang, Yun Xie, Gang Liu, Jing Wang, Honghong Lin, Yan Xin, and Junrui Zhai. "Water Use Efficiency of Soybean under Water Stress in Different Eroded Soils." Water 12, no. 2 (January 30, 2020): 373. http://dx.doi.org/10.3390/w12020373.

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Soil erosion could change the effective storage of soil moisture and affected crop water use efficiency (WUE). To quantitative study differences in the WUE of soybean and the crop’s response to water stress for soils with different degrees of erosion in northeastern China, three erosion degrees—(1) lightly, (2) moderately and (3) severely—eroded black undisturbed soils and four years (from 2013 to 2016) of soybean pot experiments were used to control soil water content (100%, 80%, 60%, and 40% field capacity (FC)) and observe the crop growth processes. To study the relationships between erosio

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Orlowski, Natalie, Lutz Breuer, Nicolas Angeli, Pascal Boeckx, Christophe Brumbt, Craig S. Cook, Maren Dubbert, et al. "Inter-laboratory comparison of cryogenic water extraction systems for stable isotope analysis of soil water." Hydrology and Earth System Sciences 22, no. 7 (July 6, 2018): 3619–37. http://dx.doi.org/10.5194/hess-22-3619-2018.

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Abstract. For more than two decades, research groups in hydrology, ecology, soil science, and biogeochemistry have performed cryogenic water extractions (CWEs) for the analysis of δ2H and δ18O of soil water. Recent studies have shown that extraction conditions (time, temperature, and vacuum) along with physicochemical soil properties may affect extracted soil water isotope composition. Here we present results from the first worldwide round robin laboratory intercomparison. We test the null hypothesis that, with identical soils, standards, extraction protocols, and isotope analyses, cryogenic e

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Barbour, S. Lee. "Nineteenth Canadian Geotechnical Colloquium: The soil-water characteristic curve: a historical perspective." Canadian Geotechnical Journal 35, no. 5 (October 1, 1998): 873–94. http://dx.doi.org/10.1139/t98-040.

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The constitutive relationship between water content or degree of saturation and suction is called the soil-water characteristic curve. The soil-water characteristic curve provides a conceptual framework in which the behavior of unsaturated soils can be understood. A historical review illustrates how the work of early researchers in soil science and geotechnical engineering laid the foundation for our current understanding of this relationship. Key elements of these early studies were a conceptual understanding of the soil-water characteristic curve as a relationship between the mass or volume

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Centeri, Csaba. "Soil Water Erosion." Water 14, no. 3 (February 1, 2022): 447. http://dx.doi.org/10.3390/w14030447.

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Ahuchaogu, Israel, Precious Ehiomogue, and Unwana Udoumoh. "Effects of soil and water conservation measures on the environment: A review." Poljoprivredna tehnika 47, no. 3 (2022): 42–55. http://dx.doi.org/10.5937/poljteh2203042a.

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The preservation and sustainable development of soil and water resources is one of the basic principles for the development of the environment. Soil degradation was a significant global issues during the 20th century and remains of high importance in the 21 st century as it affect the environment, agronomic production, food security, and quality of life. This review provides an extensive review information on soil conservation strategies or methods and their applications. Based on this, the most promising soil conservation technologies are identified to improve the management and conservation

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Ariyanto, Sandy Vikki, and Imron Rosyadi NR. "KKN-PPM: Improvement of Creativity Processing Purple Uwi into Purple Uwi Chips." Jurnal Pengabdian kepada Masyarakat (Indonesian Journal of Community Engagement) 6, no. 1 (March 31, 2020): 01. http://dx.doi.org/10.22146/jpkm.48581.

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Based on observations by DPL and KKN students of Madura University, Blaban Village is located on a plateau of rocks that make it difficult to grow plants. The soil condition of Blaban village is barren and dry during the dry season, during the rainy season the soil is cracked so that it needs water absorption to collect rainwater in the soil and improve the structure of the dry soil during the dry season. With a combination of science from soil structure (Geophysical Science), water supply in the soil (Geophysical Science), liquid fertilizer (Agricultural Science), product processing (Industri

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Gomboš, Milan. "Soil water regime in clay-loam soils." Cereal Research Communications 35, no. 2 (June 2007): 417–20. http://dx.doi.org/10.1556/crc.35.2007.2.63.

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Ahmad Bhat, Shakeel, Alban Kuriqi, Mehraj U. Din Dar, Owais Bhat, Saad Sh Sammen, Abu Reza Md Towfiqul Islam, Ahmed Elbeltagi, et al. "Application of Biochar for Improving Physical, Chemical, and Hydrological Soil Properties: A Systematic Review." Sustainability 14, no. 17 (September 5, 2022): 11104. http://dx.doi.org/10.3390/su141711104.

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Biochar is a carbon-based substance made by the pyrolysis of organic waste. The amount of biochar produced is determined by the type of feedstock and pyrolysis conditions. Biochar is frequently added to the soil for various reasons, including carbon sequestration, greenhouse gas mitigation, improved crop production by boosting soil fertility, removing harmful contaminants, and drought mitigation. Biochar may also be used for waste management and wastewater treatment. Biochar’s various advantages make it a potentially appealing instrument material for current science and technology. Although bi

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Orlowski, N., P. Kraft, and L. Breuer. "Exploring water cycle dynamics through sampling multitude stable water isotope pools in a small developed landscape of Germany." Hydrology and Earth System Sciences Discussions 12, no. 2 (February 6, 2015): 1809–53. http://dx.doi.org/10.5194/hessd-12-1809-2015.

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Abstract. Conducting a dual stable water isotope (δ2H and δ18O) study in the developed landscape of the Schwingbach catchment (Germany) helped to unravel connectivity and disconnectivity between the different water cycle components. The two-year weekly to biweekly measurements of precipitation, stream, and groundwater isotopes revealed that surface and groundwater are decoupled from the annual precipitation cycle but showed bidirectional interactions between each other. Seasonal variations based on temperature effects were observed in the precipitation signal but neither reflected in stream no

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Cresswell, HP, DE Smiles, and J. Williams. "Soil structure, soil hydraulic properties and the soil water balance." Soil Research 30, no. 3 (1992): 265. http://dx.doi.org/10.1071/sr9920265.

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We review the influence of soil structural change on the fundamental soil hydraulic properties (unsaturated hydraulic conductivity and the soil moisture characteristic) and utilize deterministic modelling to assess subsequent effects on the soil water balance. Soil structure is reflected in the 0 to -100 kPa matric potential section of the soil moisture characteristic with marked changes often occurring in light to medium textured soils' (sands, sandy-loam, loams and clay-loams). The effect of long-term tillage on soil structure may decrease hydraulic conductivity within this matric potential

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