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Journal articles on the topic 'Soil-water dynamics'

Author: Grafiati

Published: 4 June 2021

Last updated: 20 February 2023

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1

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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2

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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3

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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4

Kanda, Edwin Kimutai, Aidan Senzanje, and Tafadzwanashe Mabhaudhi. "Soil water dynamics under Moistube irrigation." Physics and Chemistry of the Earth, Parts A/B/C 115 (February 2020): 102836. http://dx.doi.org/10.1016/j.pce.2020.102836.

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5

Di Prima, Simone, Mirko Castellini, Mario Pirastru, and Saskia Keesstra. "Soil Water Conservation: Dynamics and Impact." Water 10, no. 7 (July 18, 2018): 952. http://dx.doi.org/10.3390/w10070952.

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Human needs like food and clean water are directly related to good maintenance of healthy and productive soils. A good understanding of human impact on the natural environment is therefore necessary to preserve and manage soil and water resources. This knowledge is particularly important in semi-arid and arid regions, where the increasing demands on limited water supplies require urgent efforts to improve water quality and water use efficiency. It is important to keep in mind that both soil and water are limited resources. Thus, wise use of these natural resources is a fundamental prerequisite

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6

Laczová, Elena, and Vlasta Štekauerová. "Soil water dynamics of the hillside." Cereal Research Communications 35, no. 2 (June 2007): 705–8. http://dx.doi.org/10.1556/crc.35.2007.2.135.

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7

Jong Van Uer, Q. de. "The critical soil water content and its relation to soil water dynamics." Scientia Agricola 54, spe (June 1997): 45–50. http://dx.doi.org/10.1590/s0103-90161997000300009.

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Using an edaphic model that describes the extraction of soil water by plant roots, the occurrence of depletion zones dose to plant roots is demonstrated. These depletion zones affect the root water potential that is needed to maintain a certain transpiration rate. The results show how the critical soil water content depends on soil's hydraulic properties, transpiration rate and root density.

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8

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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9

Rueedi, J. "Soil Water Dynamics, by A.W. Warrick, 2003." Environmentalist 24, no. 1 (March 2004): 59–60. http://dx.doi.org/10.1023/b:envr.0000046450.62059.62.

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10

Sharma, Sudhirendar, M. H. Fulekar, C. P. Jayalakshmi, and Conrad P. Straub. "Fly ash dynamics in soil‐water systems." Critical Reviews in Environmental Control 19, no. 3 (January 1989): 251–75. http://dx.doi.org/10.1080/10643388909388367.

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11

Kisekka, Isaya, K. W. Migliaccio, R. Muñoz-Carpena, B. Schaffer, and Y. Khare. "Modelling soil water dynamics considering measurement uncertainty." Hydrological Processes 29, no. 5 (March 17, 2014): 692–711. http://dx.doi.org/10.1002/hyp.10173.

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12

Br�da, N., A. Granier, F. Barataud, and C. Moyne. "Soil water dynamics in an oak stand." Plant and Soil 172, no. 1 (May 1995): 17–27. http://dx.doi.org/10.1007/bf00020856.

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Barataud, F., C. Moyne, N. Br�da, and A. Granier. "Soil water dynamics in an oak stand." Plant and Soil 172, no. 1 (May 1995): 29–43. http://dx.doi.org/10.1007/bf00020857.

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14

Diehl, Dörte. "Soil water repellency: Dynamics of heterogeneous surfaces." Colloids and Surfaces A: Physicochemical and Engineering Aspects 432 (September 2013): 8–18. http://dx.doi.org/10.1016/j.colsurfa.2013.05.011.

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15

Heitman, J. L., R. Horton, T. J. Sauer, and T. M. DeSutter. "Sensible Heat Observations Reveal Soil-Water Evaporation Dynamics." Journal of Hydrometeorology 9, no. 1 (February 1, 2008): 165–71. http://dx.doi.org/10.1175/2007jhm963.1.

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Abstract Soil-water evaporation is important at scales ranging from microbial ecology to large-scale climate. Yet routine measurements are unable to capture rapidly shifting near-surface soil heat and water processes involved in soil-water evaporation. The objective of this study was to determine the depth and location of the evaporation zone within soil. Three-needle heat-pulse sensors were used to monitor soil heat capacity, thermal conductivity, and temperature below a bare soil surface in central Iowa during natural wetting/drying cycles. Soil heat flux and changes in heat storage were cal

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16

Han, Jiang Bo, and Zhi Fang Zhou. "Comparison between Soil Water Dynamics Simulated by the Isothermal and Non-Isothermal Models." Advanced Materials Research 864-867 (December 2013): 2298–301. http://dx.doi.org/10.4028/www.scientific.net/amr.864-867.2298.

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To obtain a better understanding of the role of non-isothermal flow in the unsaturated zone in the presence of the water table, the isothermal and non-isothermal models driven by the observed atmospheric data were used to reproduce soil moisture dynamics observed in the lysimeter with a 100-cm water table level over one year period. Results from the simulations indicated that although the isothermal and non-isothermal models both captured the general trend of soil water content dynamics during one year period, simulated values by the isothermal model presented less dynamic variations, which ov

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17

Lapen, David R., Jonathan S. Price, and Robert Gilbert. "Soil water storage dynamics in peatlands with shallow water tables." Canadian Journal of Soil Science 80, no. 1 (February 1, 2000): 43–52. http://dx.doi.org/10.4141/s99-007.

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Time domain reflectometry (TDR) was used to estimate soil water storage dynamics in several uncultivated blanket bogs and poor fens in southeastern Newfoundland during the summer growing season. The purpose of the research was to evaluate links between surface moisture conditions, evapotranspiration, and recharge processes in order to elucidate factors that govern blanket peat formation in the region. Water storage changes in the peat/Sphagnum above the water table (ΔSWS) were found to be important storage terms in daily water balance estimates. Daily mean ΔSWS values for bog and fen approxima

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18

Jeanneau, Laurent, Pauline Buysse, Marie Denis, Gérard Gruau, Patrice Petitjean, Anne Jaffrézic, Chris Flechard, and Valérie Viaud. "Water Table Dynamics Control Carbon Losses from the Destabilization of Soil Organic Matter in a Small, Lowland Agricultural Catchment." Soil Systems 4, no. 1 (December 20, 2019): 2. http://dx.doi.org/10.3390/soilsystems4010002.

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The biogeochemistry of soil organic matter (SOM) is driven by a combination of stabilization and destabilization mechanisms. Among the various ways in which SOM is lost, soil moisture controls the leaching of dissolved organic and inorganic carbon (DOC and DIC) and CO2 fluxes (FCO2). The aim of this study was to investigate the impact of naturally occurring water table dynamics on the couplings between these three types of C losses. The DIC and DOC concentrations in the soil solutions and the FCO2 values at the soil surface were collected fortnightly over a nine-month period at four sampling p

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19

Flerchinger, G. N., M. S. Seyfried, and S. P. Hardegree. "Using Soil Freezing Characteristics to Model Multi-Season Soil Water Dynamics." Vadose Zone Journal 5, no. 4 (November 2006): 1143–53. http://dx.doi.org/10.2136/vzj2006.0025.

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20

Polyakov, V., and R. Lal. "Modeling soil organic matter dynamics as affected by soil water erosion." Environment International 30, no. 4 (June 2004): 547–56. http://dx.doi.org/10.1016/j.envint.2003.10.011.

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21

Bradley, Chris, Mary Mosugu, and John Gerrard. "Seasonal dynamics of soil–water pressure in a cracking clay soil." CATENA 69, no. 3 (April 2007): 253–63. http://dx.doi.org/10.1016/j.catena.2006.06.004.

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22

Lubana, Prit Pal Singh, and N. K. Narda. "Soil water dynamics model for trickle irrigated tomatoes." Agricultural Water Management 37, no. 2 (July 1998): 145–61. http://dx.doi.org/10.1016/s0378-3774(98)00035-3.

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23

Carminati, Andrea, Ahmad B. Moradi, Doris Vetterlein, Peter Vontobel, Eberhard Lehmann, Ulrich Weller, Hans-Jörg Vogel, and Sascha E. Oswald. "Dynamics of soil water content in the rhizosphere." Plant and Soil 332, no. 1-2 (January 23, 2010): 163–76. http://dx.doi.org/10.1007/s11104-010-0283-8.

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24

Ward, P. R., R. A. Lawes, and D. Ferris. "Soil-water dynamics in a pasture-cropping system." Crop and Pasture Science 65, no. 10 (2014): 1016. http://dx.doi.org/10.1071/cp14046.

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Pasture cropping is a farming system in which annual crops are sown into established perennial pastures. It may provide environmental benefits such as increased groundcover and reduced deep drainage, while allowing traditional crop production in the Mediterranean-style climate of south-western Australia. In this research, we investigated deep drainage and the temporal patterns of water use by a subtropical perennial grass, annual crops, and a pasture-cropping system over a 4-year period. Both the pasture and pasture-cropped treatments reduced deep drainage significantly, by ~50 mm compared wit

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25

Wan, Changgui, Ibrahim Yilmaz, and Ronald E. Sosebee. "Seasonal soil–water availability influences snakeweed root dynamics." Journal of Arid Environments 51, no. 2 (June 2002): 255–64. http://dx.doi.org/10.1006/jare.2001.0942.

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26

Young, Michael H., Lynn F. Fenstermaker, and Jayne Belnap. "Monitoring water content dynamics of biological soil crusts." Journal of Arid Environments 142 (July 2017): 41–49. http://dx.doi.org/10.1016/j.jaridenv.2017.03.004.

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27

Jiménez-de-Santiago, Lidón, and Bosch-Serra. "Soil Water Dynamics in a Rainfed Mediterranean Agricultural System." Water 11, no. 4 (April 17, 2019): 799. http://dx.doi.org/10.3390/w11040799.

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Rainfed Mediterranean agriculture is characterized by low water input and by soil water content below its field capacity during most of the year. However, erratic rainfall distribution can lead to deep drainage. The understanding of soil-water dynamics is essential to prevent collateral impacts in subsuperficial waters by leached pollutants and to implement suitable soil management (e.g., agronomic measures to avoid nitrate leaching). Soil water dynamics during two fallow years and three barley crop seasons was evaluated using the Leaching estimation and chemistry model in a semiarid Mediterra

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28

Girona, J., M. Mata, E. Fereres, D. A. Goldhamer, and M. Cohen. "Evapotranspiration and soil water dynamics of peach trees under water deficits." Agricultural Water Management 54, no. 2 (March 2002): 107–22. http://dx.doi.org/10.1016/s0378-3774(01)00149-4.

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29

Farkas, C., A. Hagyó, E. Horváth, and G. Várallyay. "A Chernozem soil water regime response to predicted climate change scenarios." Soil and Water Research 3, Special Issue No. 1 (June 30, 2008): S58—S67. http://dx.doi.org/10.17221/1410-swr.

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Climate, hydrology and vegetation are closely linked at local, regional and global scales. The recent land use and plant production systems are adapted to the present climatic conditions. Thus, studies on the influence of possible climate change scenarios on the water and heat regimes of the soil-plant-atmosphere system are important in order to work out plant production strategies, adjusted to changed conditions. In this study the effect of two possible climate change scenarios on the soil water regime of a Chernozem soil was estimated for a Hungarian site. Soil water content dynamics simulat

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30

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 16, no. 5 (May 15, 2012): 1401–17. http://dx.doi.org/10.5194/hess-16-1401-2012.

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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 from field measurements of snow hydrology and subsurface hydrologic and temperature responses during the

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31

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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32

Klenk, P., S. Jaumann, and K. Roth. "Quantitative high-resolution observations of soil water dynamics in a complicated architecture using time-lapse ground-penetrating radar." Hydrology and Earth System Sciences 19, no. 3 (March 2, 2015): 1125–39. http://dx.doi.org/10.5194/hess-19-1125-2015.

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Abstract. High-resolution time-lapse ground-penetrating radar (GPR) observations of advancing and retreating water tables can yield a wealth of information about near-surface water content dynamics. In this study, we present and analyze a series of imbibition, drainage and infiltration experiments that have been carried out at our artificial ASSESS test site and observed with surface-based GPR. The test site features a complicated but known subsurface architecture constructed with three different kinds of sand. It allows the study of soil water dynamics with GPR under a wide range of different

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33

Klenk, P., S. Jaumann, and K. Roth. "Quantitative high-resolution observations of soil water dynamics in a complicated architecture with time-lapse Ground-Penetrating Radar." Hydrology and Earth System Sciences Discussions 11, no. 11 (November 4, 2014): 12365–404. http://dx.doi.org/10.5194/hessd-11-12365-2014.

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Abstract. High-resolution time-lapse Ground-Penetrating Radar (GPR) observations of advancing and retreating water tables can yield a wealth of information about near-surface water content dynamics. In this study, we present and analyze a series of imbibition, drainage and infiltration experiments which have been carried out at our artificial ASSESS test site and observed with surface based GPR. The test site features a complicated but known subsurface architecture constructed with three different kinds of sand. It allows studying soil water dynamics with GPR under a wide range of different co

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34

Lebon, Eric, Vincent Dumas, Philippe Pieri, and Hans R. Schultz. "Modelling the seasonal dynamics of the soil water balance of vineyards." Functional Plant Biology 30, no. 6 (2003): 699. http://dx.doi.org/10.1071/fp02222.

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A geometrical canopy model describing radiation absorption (Riou et al. 1989, Agronomie 9, 441–450) and partitioning between grapevines (Vitis vinifera L.) and soil was coupled to a soil water balance routine describing a bilinear change in relative transpiration rate as a function of the fraction of soil transpirable water (FTSW). The model was amended to account for changes in soil evaporation after precipitation events and subsequent dry-down of the top soil layer. It was tested on two experimental vineyards in the Alsace region, France, varying in soil type, water-holding capacity and root

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35

Couvreur, V., J. Vanderborght, L. Beff, and M. Javaux. "Horizontal soil water potential heterogeneity: simplifying approaches for crop water dynamics models." Hydrology and Earth System Sciences 18, no. 5 (May 12, 2014): 1723–43. http://dx.doi.org/10.5194/hess-18-1723-2014.

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Abstract. Soil water potential (SWP) is known to affect plant water status, and even though observations demonstrate that SWP distribution around roots may limit plant water availability, its horizontal heterogeneity within the root zone is often neglected in hydrological models. As motive, using a horizontal discretisation significantly larger than one centimetre is often essential for computing time considerations, especially for large-scale hydrodynamics models. In this paper, we simulate soil and root system hydrodynamics at the centimetre scale and evaluate approaches to upscale variables

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36

Couvreur, V., J. Vanderborght, L. Beff, and M. Javaux. "Horizontal soil water potential heterogeneity: simplifying approaches for crop water dynamics models." Hydrology and Earth System Sciences Discussions 11, no. 1 (January 23, 2014): 1203–52. http://dx.doi.org/10.5194/hessd-11-1203-2014.

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Abstract. Soil water potential (SWP) is known to affect plant water status, and even though observations demonstrate that SWP distribution around roots may limit plant water availability, its horizontal heterogeneity within the root zone is often neglected in hydrological models. As motive, using a horizontal discretisation significantly larger than one centimetre is often essential for computing time considerations, especially for large scale hydrodynamics models. In this paper, we simulate soil and root system hydrodynamics at the centimetre scale and evaluate approaches to upscale variables

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37

Zhang, Minghe, Xuan Feng, Maksim Bano, Huiting Xing, Taihan Wang, Wenjing Liang, Haoqiu Zhou, Zejun Dong, Yafei An, and Yinghao Zhang. "Review of Ground Penetrating Radar Applications for Water Dynamics Studies in Unsaturated Zone." Remote Sensing 14, no. 23 (November 26, 2022): 5993. http://dx.doi.org/10.3390/rs14235993.

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For water dynamics investigation in unsaturated (vadose) zones, ground penetrating radar is a popular hydro-geophysical method because it is non-invasive for soil, has high resolution and the results have a direct link with water content. Soil water content and soil hydraulic properties are two key factors for describing the water dynamics in vadose zones. There has been tremendous progress in soil water content and soil hydraulic properties estimation with ground penetrating radar. The purpose of this paper is to provide an overview of the application of ground penetrating radar for soil wate

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38

Liu, Yuan Yuan, Hai Yan Sun, and Zhi Guo Zhang. "Identification and Optimization of Soil Water Movement Model Based on GA under Drip-Irrigation." Applied Mechanics and Materials 571-572 (June 2014): 148–51. http://dx.doi.org/10.4028/www.scientific.net/amm.571-572.148.

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Under drip irrigation, the drip discharge has a great influence on soil water movement and crop growth. Studying the soil water movement rules makes great realistic significance to the precise management. Based on soil dynamics theory, we measured the water movement distance of saline soil in Changji Xinjiang through outdoor tests. Then, we built transfer function models between drip discharge and water movement distance under drip irrigation and applied the genetic algorithm to identifying and optimizing model’s parameters. Comparing the soil water movement model’s dynamic change at the same

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39

Bonini da Luz, Felipe, Martha Lustosa Carvalho, Daniel Aquino de Borba, Bruna Emanuele Schiebelbein, Renato Paiva de Lima, and Maurício Roberto Cherubin. "Linking Soil Water Changes to Soil Physical Quality in Sugarcane Expansion Areas in Brazil." Water 12, no. 11 (November 12, 2020): 3156. http://dx.doi.org/10.3390/w12113156.

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Brazil is the world’s largest sugarcane producer with projections for expanding the current area by 30% in the coming years, mainly in areas previously occupied by pastures. We assess soil water changes induced by land-use change (LUC) for sugarcane expansion in the central-south region of Brazil. For that purpose, soil samples were collected in a typical LUC sequence (native vegetation–pasture–sugarcane) in two contrasting soil textures (i.e., sandy and clayey). Soil hydro-physical properties such as pores size distribution, bulk density, soil water content, water tension, and drainage time a

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40

Liu, Bingxia, and Ming’an Shao. "Modeling soil–water dynamics and soil–water carrying capacity for vegetation on the Loess Plateau, China." Agricultural Water Management 159 (September 2015): 176–84. http://dx.doi.org/10.1016/j.agwat.2015.06.019.

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41

Modise, David M., Michael D. Glenn, and Morris Ingle. "THE DYNAMICS OF HYDRAULIC LIFT IN PEACH TREE." HortScience 30, no. 2 (April 1995): 187b—187. http://dx.doi.org/10.21273/hortsci.30.2.187b.

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The split root technique was used to study water afflux in peach [Prunus persica (L.) Batsch] from wet to dry soil through root systems that bridge wet and dry soil. Peach trees conduct hydraulic lift (HL) to ameliorate water deficits in dry soil layers, under conditions of low transpirational demand. The objectives of this study were to examine the magnitude of HL in peach and to determine its effect on nutrient uptake from dry soil. In addition, the split root system was used to measure peach water uptake from soil supporting `Kentucky 31' tall fescue [Festuca arundinaceae (Schreb)] and dete

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42

Nielsen, Christian, Oliver Bühler, and Palle Kristoffersen. "Soil Water Dynamics and Growth of Street and Park Trees." Arboriculture & Urban Forestry 33, no. 4 (July 1, 2007): 231–45. http://dx.doi.org/10.48044/jauf.2007.027.

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Soil water dynamics were studied in 100 street tree planting pits and in the soil surrounding five park trees. Volumetric soil water content and stem cross-sectional area increment were measured on both park and street trees. Different levels of irrigation were implemented on the 100 street trees. Winter assessments of soil wetness at field capacity showed that the water retention capacity was lower in street planting pits than in the park soil attributable to the rather coarse substrate used in the planting pits. High variability among street tree planting pits in regard to water retention ca

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43

Šimanský, Vladimír, and Peter Kováčik. "Carbon sequestration and its dynamics in water-stable aggregates." Agriculture (Pol'nohospodárstvo) 60, no. 1 (March 1, 2014): 1–9. http://dx.doi.org/10.2478/agri-2014-0001.

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Abstract Sequestration of organic carbon in soils is an effective strategy to mitigate global climate change. Carbon sequestration leads to an increase in carbon stocks in soil, thereby reducing greenhouse gas emissions while improving soil quality and crop production. There are several published articles containing information in which the authors explain carbon sequestration in different soil types under different climatic conditions or farming systems, but on the other hand there is less information about carbon sequestration in water-stable aggregates. In field experiment, the manner in wh

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44

Musinovich, Sarimsakov Maksudkhon, and Kimsanov Ibrahim Khaitmuratovich. "The Determination Of Soil Moisturization Dynamics Four Factor Experience." American Journal of Interdisciplinary Innovations and Research 03, no. 11 (November 13, 2021): 1–8. http://dx.doi.org/10.37547/tajiir/volume03issue11-01.

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This article presents the data of a four-factor experiment to determine the soil moisture perimeter in the field of drip irrigation in intensive gardening and to further increase the efficiency of water use.

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45

Ket, Pinnara, Chantha Oeurng, and Aurore Degré. "Estimating Soil Water Retention Curve by Inverse Modelling from Combination of In Situ Dynamic Soil Water Content and Soil Potential Data." Soil Systems 2, no. 4 (October 2, 2018): 55. http://dx.doi.org/10.3390/soilsystems2040055.

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Soil water retention curves (SWRCs) are crucial for characterizing soil moisture dynamics, and are particularly relevant in the context of irrigation management. Inverse modelling is one of the methods used to parameterize models representing these curves, which are closest to the field reality. The objective of this study is to estimate the soil hydraulic properties through inverse modelling using the HYDRUS-1D code based on soil moisture and potential data acquired in the field. The in situ SWRCs acquired every 30 min are based on simultaneous soil water content and soil water potential meas

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46

Ngan, Nguyen Vo Chau, Huynh Van Thao, and Nguyen Dinh Giang Nam. "Nutrient dynamics in water and soil under conventional rice cultivation in the Vietnamese Mekong Delta." F1000Research 10 (January 5, 2023): 1145. http://dx.doi.org/10.12688/f1000research.73904.2.

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Background The evaluation of nutrient variability plays a crucial role in accessing soil potentials and practical intervention responses in rice production systems. Synthetic fertilizer applications and cultivation practices are considered key factors affecting nutrient dynamics and availability. Here, we assessed the nutrient dynamics in surface, subsurface water and soil under local water management and conventional rice cultivation practices in the Vietnamese Mekong Delta. Methods We implemented a field experiment (200 m 2) in the 2018 wet season and the 2019 dry season in a triple rice-cro

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47

Carrera, Alberto, Matteo Longo, Ilaria Piccoli, Benjamin Mary, Giorgio Cassiani, and Francesco Morari. "Electro-Magnetic Geophysical Dynamics under Conservation and Conventional Farming." Remote Sensing 14, no. 24 (December 9, 2022): 6243. http://dx.doi.org/10.3390/rs14246243.

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In the context of global warming, agriculture faces severe challenges such as water scarcity and soil erosion. Key to achieving soil sustainability is the choice of farming practices, the consequences of which are generally site-specific. In this study, the ability of Electrical Resistivity Tomography (ERT) and Electro Magnetic Induction (EMI) methods were assessed for monitoring the effects of conventional (CONV) and conservation (CONS) agricultural practices. The aim is to highlight differences in soil water distribution caused by both short- and long-term effects of the two different practi

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Smith, Aaron, Doerthe Tetzlaff, Hjalmar Laudon, Marco Maneta, and Chris Soulsby. "Assessing the influence of soil freeze–thaw cycles on catchment water storage–flux–age interactions using a tracer-aided ecohydrological model." Hydrology and Earth System Sciences 23, no. 8 (August 13, 2019): 3319–34. http://dx.doi.org/10.5194/hess-23-3319-2019.

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Abstract. Ecohydrological models are powerful tools to quantify the effects that independent fluxes may have on catchment storage dynamics. Here, we adapted the tracer-aided ecohydrological model, EcH2O-iso, for cold regions with the explicit conceptualization of dynamic soil freeze–thaw processes. We tested the model at the data-rich Krycklan site in northern Sweden with multi-criterion calibration using discharge, stream isotopes and soil moisture in three nested catchments. We utilized the model's incorporation of ecohydrological partitioning to evaluate the effect of soil frost on evaporat

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Sławiński, C., J. Cymerman, B. Witkowska-Walczak, and K. Lamorski. "Impact of diverse tillage on soil moisture dynamics." International Agrophysics 26, no. 3 (July 1, 2012): 301–9. http://dx.doi.org/10.2478/v10247-012-0043-5.

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Impact of diverse tillage on soil moisture dynamicsThe influences of traditional and reduced tillage on the water content dynamics of two soils were investigated in a long-term field experiment under nearly the same meteorological conditions for a winter wheat monoculture during three years. In addition to the moisture changes, the basic physicochemical properties, water retention, differential porosity and hydraulic conductivity of the investigated soils were measured. The results have shown the dependence between moisture and the tillage system applied for both types of soil. The soil water

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Sala, O. E., W. K. Lauenroth, and W. J. Parton. "Long-Term Soil Water Dynamics in the Shortgrass Steppe." Ecology 73, no. 4 (August 1992): 1175–81. http://dx.doi.org/10.2307/1940667.

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