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1

Shelia, Vakhtang, Jirka Šimůnek, Ken Boote, and Gerrit Hoogenbooom. "Coupling DSSAT and HYDRUS-1D for simulations of soil water dynamics in the soil-plant-atmosphere system." Journal of Hydrology and Hydromechanics 66, no. 2 (2018): 232–45. http://dx.doi.org/10.1515/johh-2017-0055.

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AbstractAccurate estimation of the soil water balance of the soil-plant-atmosphere system is key to determining the availability of water resources and their optimal management. Evapotranspiration and leaching are the main sinks of water from the system affecting soil water status and hence crop yield. The accuracy of soil water content and evapotranspiration simulations affects crop yield simulations as well. DSSAT is a suite of field-scale, process-based crop models to simulate crop growth and development. A “tipping bucket” water balance approach is currently used in DSSAT for soil hydrolog
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Gao, Hongfei, and Hao Hong. "Study on the Transport Mechanism of Soil Water Ions in Unsaturated Zone." Academic Journal of Science and Technology 2, no. 3 (2022): 10–13. http://dx.doi.org/10.54097/ajst.v2i3.1436.

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In order to understand the law of solute transport in the unsaturated zone, this paper selects a beach of the Yellow River in jiaozuo area as the study area, and uses Hydrus software to simulate some typical hydrochemical ions in the unsaturated zone. The Hydrus software is a numerical model developed by the National Saline soil Improvement Center in 1991 for simulating water, energy and solute transport in variably saturated porous media. Hydrus-1d is a one-dimensional version of the Hydrus software, which is commonly used to simulate water and solutes. The results show that Hydrus-1D can sim
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3

Nascimento, Ícaro Vasconcelos do, Raimundo Nonato de Assis Júnior, José Carlos de Araújo, et al. "Estimation of van Genuchten Equation Parameters in Laboratory and through Inverse Modeling with Hydrus-1D." Journal of Agricultural Science 10, no. 3 (2018): 102. http://dx.doi.org/10.5539/jas.v10n3p102.

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Soil water retention curve (SWRC) becomes important because it guides when and how much to irrigate, optimizing the use of water; can be obtained in the field or laboratory, being commonly determined in the laboratory with porous plate apparatus, and the determination is compromised by issues such as time and labor. In this context, inverse modeling emerges, which allows to obtain a variable going from the effect to the cause, using Hydrus-1D. Hence, this study aims to obtain van Genuchten equation parameters through inverse modeling with Hydrus-1D and make the respective comparisons and infer
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Kim, Hwansuk, Haein Sim, Seungwan Hong, et al. "Comparative Evaluation of Evapotranspiration and Optimization Schemes for Green Roof Runoff Simulations Using HYDRUS-1D." Water 16, no. 19 (2024): 2835. http://dx.doi.org/10.3390/w16192835.

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The use of green roofs, a low-impact development practice, can be an effective means of reducing direct runoff in urban centers. Green roof modeling can enable efficient design by preliminarily grasping the behavior of the green roof system according to specific configurations. In this study, we aimed to find appropriate evapotranspiration and parameter optimization schemes for HYDRUS-1D, a commonly used modeling tool for green roofs. Comparative studies of this sort in the context of green roof runoff modeling have not been conducted previously and are important in guiding users to overcome t
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Melo, Cristiane Ribeiro de, Paulo Abadie Guedes, Samuel França Amorim, Fellipe Henrique Borba Alves, and José Almir Cirilo. "Combined analysis of landslide susceptibility and soil water dynamics in a metropolitan area, northeast Brazil." Soils and Rocks 44, no. 2 (2021): 1–14. http://dx.doi.org/10.28927/sr.2021.051420.

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Landslide susceptibility and water balance in the soil, in the community of Lagoa Encantada, Recife Metropolitan Area, Brazil, were assessed using the computational models SINMAP and HYDRUS-1D. The SINMAP input parameters were the physical and hydrodynamic characteristics of the soil, evidence of landslides and the DEM; and for the HYDRUS-1D model, the hydraulic parameters of the soil. For both programs, simulations were also carried out, based on the rain recorded in the area. The soil was classified using the Unified Soil Classification System (USCS). To assess infiltration processes that ca
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6

Saso, J. K., G. W. Parkin, C. F. Drury, J. D. Lauzon, and W. D. Reynolds. "Chloride leaching in two Ontario soils: Measurement and prediction using HYDRUS-1D." Canadian Journal of Soil Science 92, no. 2 (2012): 285–96. http://dx.doi.org/10.4141/cjss2011-046.

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Saso, J. K., Parkin, G. W., Drury, C. F., Lauzon, J. D. and Reynolds, W. D. 2012. Chloride leaching in two Ontario soils: Measurement and prediction using HYDRUS-1D. Can. J. Soil Sci. 92: 285–296. Deterministic numerical modelling can often be used to complement and extend field results, and to provide extra insight into the mechanisms of water and solute movement within the profile of agricultural soils. Chloride leaching and near-surface soil water content in a Guelph loam and a Maryhill loam cropped to corn (Zea mays L.) were measured over a 12-mo period (October 2007 to September 2008) and
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7

Haowen, Xie, Wu Yawen, Wang Luping, et al. "Comparing simulations of green roof hydrological processes by SWMM and HYDRUS-1D." Water Supply 20, no. 1 (2019): 130–39. http://dx.doi.org/10.2166/ws.2019.140.

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Abstract Green roofs are a sustainable, low-impact development technique. They can reduce peak stormwater runoff and runoff volume and improve the quality of runoff from individual buildings and developments, which can lower the risk of frequent urban flooding and improve the quality of receiving waters. Few studies have compared different types of green roof models under the same rainfall intensities; thus, in this study, the predictions of a non-linear storage reservoirs model, Storm Water Management Model (SWMM), and a physical process model (HYDRUS-1D) were discussed. Both models were comp
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8

Sutanto, S. J., J. Wenninger, A. M. J. Coenders-Gerrits, and S. Uhlenbrook. "Partitioning of evaporation into transpiration, soil evaporation and interception: a comparison between isotope measurements and a HYDRUS-1D model." Hydrology and Earth System Sciences 16, no. 8 (2012): 2605–16. http://dx.doi.org/10.5194/hess-16-2605-2012.

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Abstract. Knowledge of the water fluxes within the soil-vegetation-atmosphere system is crucial to improve water use efficiency in irrigated land. Many studies have tried to quantify these fluxes, but they encountered difficulties in quantifying the relative contribution of evaporation and transpiration. In this study, we compared three different methods to estimate evaporation fluxes during simulated summer conditions in a grass-covered lysimeter in the laboratory. Only two of these methods can be used to partition total evaporation into transpiration, soil evaporation and interception. A wat
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Tárník, Andrej, and Dušan Igaz. "Validation of Hydrus 1D Model in Selected Catchment of Slovakia." Acta Horticulturae et Regiotecturae 20, no. 1 (2017): 24–27. http://dx.doi.org/10.1515/ahr-2017-0006.

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Abstract Soil water content is very important for agricultural practice. Direct measurements of the soil moisture are being replaced by mathematical simulations and models step by step. One of the most used models for the simulation of the soil moisture is HYDRUS 1D model. This paper deals with HYDRUS 1D validity check in the Nitra River Catchment. Three different localities in the Nitra River Catchment (Malanta, Kolíňany and Dolné Naštice) were chosen for model validity check. Both, measurements and modelling of soil moisture, were made for these localities in three years (8/2011 - 8/2014). T
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Ma, Wen Cui, Xue Yi You, Xin Xin Wang, and Yu Chen. "Numerical Simulation of Migration and Transformation of Petroleum Hydrocarbons in Soils." Advanced Materials Research 1073-1076 (December 2014): 653–56. http://dx.doi.org/10.4028/www.scientific.net/amr.1073-1076.653.

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Considering the diffusion, adsorption or desorption, and microbial degradation of petroleum hydrocarbons (PHs) in the soil–water system, the numerical model describing the migration and transportation of PHs is estabilished and it is simulated by HYDRUS-1D model. The degradation effect of time and depth variation of PHs is gained by numerical simulation. The results show that the degradation ability of indigenous microbial of PHs is poor. The HYDRUS-1D software is feasible in simulating and predicting the migration and transformation of PHs in soils.
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11

Oad, Vipin, Adam Szymkiewicz, Tomasz Berezowski, et al. "Incorporation of Horizontal Aquifer Flow into a Vertical Vadose Zone Model to Simulate Natural Groundwater Table Fluctuations." Water 17, no. 14 (2025): 2046. https://doi.org/10.3390/w17142046.

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The main goal of our work was to evaluate approaches for modeling lateral outflow from shallow unconfined aquifers in a one-dimensional model of vertical variably-saturated flow. The HYDRUS-1D model was modified by implementing formulas representing lateral flow in an aquifer, with linear or quadratic drainage functions describing the relationship between groundwater head and flux. The results obtained by the modified HYDRUS-1D model were compared to the reference simulations with HydroGeoSphere (HGS), with explicit representation of 2D flow in unsaturated and saturated zones in a vertical cro
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Anwar, A. H. M. Faisal, and Larissa Chan Thien. "Investigating Leachate Transport at Landfill Site Using HYDRUS-1D." International Journal of Environmental Science and Development 6, no. 10 (2015): 741–45. http://dx.doi.org/10.7763/ijesd.2015.v6.691.

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13

Radka Kodešová and Lukáš, Brodský. "Comparison of CGMS-WOFOST and HYDRUS-1D Simulation Results for One Cell of CGMS-GRID50." Soil and Water Research 1, No. 2 (2013): 39–48. http://dx.doi.org/10.17221/6504-swr.

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CGMS (Crop Growth Monitoring System) developed by JRC is an integrated system to monitor crop behaviour and quantitative crop yield forecast that operates on a European scale. To simulate water balance in the root zone the simulation model CGMS-WOFOST (SUPIT & VAN DER GOOT 2003) is used that is based on water storage routing. This study was performed to assess a possible impact of simplifications of the water storage routing based model on simulated water regime in the soil profile. Results of CGMS-WOFOST are compared with results of a more precise Richards’ equation based mo
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Liu, Tiegang, Jianbin Lai, Yi Luo, and Lei Liu. "Study on extinction depth and steady water storage in root zone based on lysimeter experiment and HYDRUS-1D simulation." Hydrology Research 46, no. 6 (2015): 871–79. http://dx.doi.org/10.2166/nh.2015.191.

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HYDRUS-1D was combined with lysimeter experiments to study extinction depth and steady water storage in root zone (Ws) of groundwater evaporation (ETgw) under winter wheat and silt soil. The measured soil water contents and daily ETgw with various groundwater depths were used to calibrate and validate the parameters in HYDRUS-1D. In total, 13 groundwater depths ranging from 0.5 to 5.0 m were set up for scenario simulation to determine the extinction depth and Ws. The results showed that HYDRUS-1D had an acceptable performance in simulating the soil water storage in the 0–60 cm layer and the da
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15

Rubio, Carles M., and Rafael Poyatos. "Applicability of Hydrus-1D in a Mediterranean Mountain Area Submitted to Land Use Changes." ISRN Soil Science 2012 (February 19, 2012): 1–7. http://dx.doi.org/10.5402/2012/375842.

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The aim of this research is to evaluate the reliability and accuracy of the Hydrus-1D model to simulate the measured dynamics of water flow in a silt loam soil profile located in an abandoned crop area. The paper includes a physical and chemical characterization of the soil, and hydraulic properties characteristics as well. Several techniques and devices were used to develop the experiment in both, field and laboratory scales. The last part of the study was the Hydrus-1D simulation using real rain events and evapotranspiration rates. In summary, it could predict accurately the water dynamics o
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16

Mohiuddin, Muhammad, Jawad Ali, Megersa Kebede Leta, Muhammad Waseem, Muhammad Irshad, and Zahid Hussain. "Estimation of Iodine Leaching in Soil Amended with Organic and Inorganic Materials Using HYDRUS 1-D Model." Sustainability 13, no. 19 (2021): 10967. http://dx.doi.org/10.3390/su131910967.

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This study investigated the ability of a HYDRUS 1D model for predicting the vertical distribution of potassium iodine (200 ppm) in soil columns after amendment with five different common remediation materials (gypsum, lime, fly ash, charcoal, and sawdust) at a rate of 2.5% (w/w), relative to an unamended control soil. Results showed that relative to the unamended soil, iodine leaching was decreased by all amendments but that the magnitude of the decreases varied with the soil amendment applied. Iodine content was highest in the upper layer of the soil columns and decreased progressively with s
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17

NAZIR, NUZHAT BINT, YOGESH PANDEY, SAMEERA QAYOOM, and SUSHMITA M. DADHICH. "Modelling of moisture movement and irrigation scheduling in drip irrigated tomato using CROPWAT and HYDRUS-1D." Journal of Agrometeorology 26, no. 2 (2024): 215–19. http://dx.doi.org/10.54386/jam.v26i2.2492.

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The irrigation systems require modernization and management by evaluating water system prerequisites precisely. A study was carried out at Srinagar during kharif 2022 to determine the crop water demands, irrigation scheduling and simulation of moisture movement under different irrigation regimes on tomato crop in open field conditions using CROPWAT and HYDRUS-1D models. The results revealed that the average crop water requirement at 100% ETC per plant per day was 0.24 l plant-1 day-1 during the initial stage, 0.37 l plant-1 day-1 during development stage, 0.85 l plant-1 day-1 during mid-stage
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18

Chairani, Susi. "Modeling Nitrogen and Phosphorus Transport in Vadose Zone using HYDRUS- 1D." Rona Teknik Pertanian 6, no. 2 (2021): 465–70. http://dx.doi.org/10.17969/rtp.v6i2.20431.

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Abstract. The application of large manure on the agricultural lands that derived from the Concentrated Animal Feeding Operations (CAFOs) could cause excess nutrients such as nitrogen and phosphorus transport to the groundwater through vadose (unsaturated) zone. The objective of this study is as follows: (1) to compare nitrogen and phosphorus transport in the vadose zone at different Land Management Units (LMUs) for three consecutive years (2004-06) using HYDRUS-1D, and (2) to analyze the sensitivity of nitrogen and phosphorus transport in different soil types on the van Genuchten soil hydrauli
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19

Moghbel, Farzam, Abolfazl Mosaedi, Jonathan Aguilar, Bijan Ghahraman, Hossein Ansari, and Maria C. Gonçalves. "Uncertainty Analysis of HYDRUS-1D Model to Simulate Soil Salinity Dynamics under Saline Irrigation Water Conditions Using Markov Chain Monte Carlo Algorithm." Agronomy 12, no. 11 (2022): 2793. http://dx.doi.org/10.3390/agronomy12112793.

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Utilizing degraded quality waters such as saline water as irrigation water with proper management methods such as leaching application is a potential answer to water scarcity in agricultural systems. Leaching application requires understanding the relationship between the amount of irrigation water and its quality with the dynamic of salts in the soil. The HYDRUS-1D model can simulate the dynamic of soil salinity under saline water irrigation conditions. However, these simulations are subject to uncertainty. A study was conducted to assess the uncertainty of the HYDRUS-1D model parameters and
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20

Li, Feng, Shihong Yang, Xiyun Jiao, and Zewei Jiang. "Accumulation Patterns and Numerical Simulation of Nitrate-N in Layered Soils of the Vadose Zone in Cotton Fields." Water 17, no. 8 (2025): 1117. https://doi.org/10.3390/w17081117.

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Excessive nitrogen fertilizer in cotton cultivation boosts yields but causes groundwater pollution via nitrate-N (NO3−-N) accumulation. This study combined field experiments and HYDRUS-1D modeling to analyze water and NO3−-N dynamics in the vadose zone of cotton fields in Nanpi, Hebei Province, North China, under deep groundwater conditions. Monitoring during a 184-day growth period revealed that NO3−-N accumulation increased from 11.4 to 21.2 g m−3 under conventional flood irrigation and pre-sowing fertilization. Soil texture critically influenced peak NO3−-N accumulation depth, while rainfal
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Šimůnek, Jiří, Miroslav Šejna, and Martinus Th van Genuchten. "New features of version 3 of the HYDRUS (2D/3D) computer software package." Journal of Hydrology and Hydromechanics 66, no. 2 (2018): 133–42. http://dx.doi.org/10.1515/johh-2017-0050.

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AbstractThe capabilities of the HYDRUS-1D and HYDRUS (2D/3D) software packages continuously expanded during the last two decades. Various new capabilities were added recently to both software packages, mostly by developing new standard add-on modules such as HPx, C-Ride, UnsatChem, Wetland, Fumigant, DualPerm, and Slope Stability. The new modules may be used to simulate flow and transport processes in one- and two-dimensional transport domains and are fully supported by the HYDRUS graphical user interface (GUI). Several nonstandard add-on modules, such as Overland, Isotope, and Centrifuge, hav
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Dmytruk, Y., and V. Zakharovskyi. "Hydrus’s-1D capability for assessment of soils water regime." AgroChemistry and Soil Science, no. 89 (2020): 18–27. http://dx.doi.org/10.31073/acss89-02.

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Triptimoni Borah and Manipuspak Hazarika. "A study of the water quality parameter and its impact using HYDRUS-1D in Deepor Beel, Guwahati, Assam." World Journal of Advanced Engineering Technology and Sciences 9, no. 2 (2023): 200–205. http://dx.doi.org/10.30574/wjaets.2023.9.2.0148.

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This study focuses on knowing the status of 12 water quality parameters with their variation and soil-solute interaction due to dumping of wastes at six different locations of Deepor Beel (a Ramsar site), finding their necessary correlations and development of a solute transport model using HYDRUS-1D software. HYDRUS-1D model used in this study will show the movement of iron through the soil profile in the area selected near the Municipal dumping yard at Boragaon. The results indicated that certain parameters are higher than their standard permissible limits with its extreme values obtained at
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Arrey, I. A., J. O. Odiyo, R. Makungo, and M. O. Kataka. "Effect of hysteresis on water flow in the vadose zone under natural boundary conditions, Siloam Village case study, South Africa." Journal of Hydroinformatics 20, no. 1 (2017): 88–99. http://dx.doi.org/10.2166/hydro.2017.091.

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Abstract A one-dimensional vadose zone model was used to simulate flow under natural boundary conditions. The effects of hysteresis and temporal variability of meteorological conditions were evaluated. Simulations were performed in HYDRUS-1D code for the period April 2013–January 2014 (6601 hours) at three different locations in a delineated portion of the sub-quaternary catchment A80A of Nzhelele with different soil textures. Soil hydraulic characteristics were estimated in a Rosetta library dynamically linked to the HYDRUS-1D model which is based on the numerical solution of a one-dimensiona
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Iqbal, Mazhar, Md Rowshon Kamal, Mohd Amin Mohd Soom, et al. "HYDRUS-1D Simulation of Nitrogen Dynamics in Rainfed Sweet Corn Production." Applied Sciences 10, no. 11 (2020): 3925. http://dx.doi.org/10.3390/app10113925.

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Nitrogen loss from agricultural fields results in contamination of ground and surface water resources due to leaching and runoff, respectively. Nitrogen transport dynamics vary significantly among agricultural fields of different climates, especially in the tropical climate. This study intended to evaluate the rainfall impact on nitrogen distribution and losses under tropical rain-fed conditions. The study was carried out in a sweet corn field for two growing seasons at the Malaysian Agricultural Research and Development Institute (MARDI) research field. The HYDRUS-1D numerical model was used
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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 (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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Hilten, Roger Norris, Thomas Mark Lawrence, and Earnest William Tollner. "Modeling stormwater runoff from green roofs with HYDRUS-1D." Journal of Hydrology 358, no. 3-4 (2008): 288–93. http://dx.doi.org/10.1016/j.jhydrol.2008.06.010.

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Š;imůnek, Jirka, Diederik Jacques, Martinus Th Genuchten, and Dirk Mallants. "MULTICOMPONENT GEOCHEMICAL TRANSPORT MODELING USING HYDRUS-1D AND HP11." Journal of the American Water Resources Association 42, no. 6 (2006): 1537–47. http://dx.doi.org/10.1111/j.1752-1688.2006.tb06019.x.

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Chen, Kaiwen, Shuang’en Yu, Tao Ma, et al. "Modeling the Water and Nitrogen Management Practices in Paddy Fields with HYDRUS-1D." Agriculture 12, no. 7 (2022): 924. http://dx.doi.org/10.3390/agriculture12070924.

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Rice production involves abundant water and fertilizer inputs and is prone to nitrogen (N) loss via surface runoff and leaching, resulting in agricultural diffuse pollution. Based on a two-season paddy field experiment in Jiangsu Province, China, field water and N dynamics and their balances were determined with the well-calibrated HYDRUS-1D model. Then, scenarios of different controlled drainage and N fertilizer applications were simulated using the HYDRUS-1D model to analyze the features and factors of N loss from paddy fields. Evapotranspiration and deep percolation were the two dominant lo
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Maleknia, P., N. Ugwonoh, and S. Czigány. "Comparing the effect of various land use types on moisture dynamics in loamy soils with Hydrus-1D." IOP Conference Series: Earth and Environmental Science 1455, no. 1 (2025): 012016. https://doi.org/10.1088/1755-1315/1455/1/012016.

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Abstract The increasingly severe hydrological extremes observed over time are consequences of climate change in the Pannonian Basin. This study focuses on soil moisture (SM) patterns across three distinct land uses: pasture, Ploughland, and orchard situated in the Transdanubian Hills of southwestern Hungary. The study area is characterized by a subhumid continental climate. The study evaluates the effectiveness of the Hydrus-1D model in simulating SM in silt and silty loam soils. Gaining a deeper understanding of SM dynamics is crucial for improving soil management practices and mitigating the
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Dias, Allana Siqueira, and Willames De Albuquerque Soares. "Desempenho do modelo Hydrus - 1D utilizando diferentes formas de caracterização hidrodinâmica." Holos Environment 19, no. 3 (2019): 376. http://dx.doi.org/10.14295/holos.v19i3.12309.

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A utilização da modelagem matemática para a simulação dos eventos hidrológicos é de fundamental importância no planejamento do uso e conservação do solo, para agricultura e pecuária, na meteorologia e na gestão dos recursos hídricos, sendo uma ferramenta conveniente para a avaliação de impactos no meio ambiente devido as atividades humanas.O uso agropecuário de alguns tipos de solo (como é o caso do Neossolo Flúvico) depende de suas condições de drenagem e se são necessárias correções desse fator ou não. Condições estas, que podem ser caracterizadas com o uso de modelos computacionais, como o
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V, Chavan Vaishnavi. "Evaluation of Municipal Solid Waste Landfill by HELP Model and Leachate Modelling by Hydrus-1d: A Review." International Journal for Research in Applied Science and Engineering Technology 12, no. 12 (2024): 79–82. https://doi.org/10.22214/ijraset.2024.65712.

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The effective management of municipal solid waste (MSW) landfills is vital for minimizing their environmental and public health impacts. The Hydrologic Evaluation of Landfill Performance (HELP) model and HYDRUS-1D are widely used tools for modeling landfill hydrology and leachate dynamics, respectively. This review consolidates recent advances in their application for evaluating MSW landfills. The HELP model's capabilities in simulating landfill hydrological behavior and HYDRUS-1D’s precision in modeling leachate transport through porous media are explored. The paper highlights the advantages,
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Acharya, Bibek, Vivek Sharma, Charles Barrett, Michael D. Dukes, and Lincoln Zotarelli. "Comparing Passive Wick Lysimeter Against Soil Water Balance and Simulation Models in High and Perched Water Tables and Coarse Sandy Soils." Journal of Natural Resources and Agricultural Ecosystems 3, no. 1 (2025): 37–52. https://doi.org/10.13031/jnrae.16188.

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HighlightsPassive wick lysimeter performance was tested against soil water balance and simulation models under high and perched water table conditions.Passive wick lysimeters overestimated deep drainage as compared to soil water balance and simulation models.Lysimeter data inflated NO3-N leachate estimates, questioning the reliability in similar field conditions.The out-row placed lysimeters recorded higher drainage volumes than in-row placed.Abstract. Understanding soil water and nutrient dynamics is pivotal for agricultural and environmental research, particularly the accurate measurement of
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Zeng, Wen-Zhi, Guo-Qing Lei, Hong-Ya Zhang, et al. "Estimating Root Zone Moisture from Surface Soil Using Limited Data." Ecological Chemistry and Engineering S 24, no. 4 (2017): 501–16. http://dx.doi.org/10.1515/eces-2017-0033.

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Abstract For estimation of root-zone moisture content from EO-1/Hyperion imagery, surface soil moisture was first predicted by hyperspectral reflectance data using partial least square regression (PLSR) analysis. The textures of more than 300 soil samples extracted from a 900 m × 900 m field site located within the Hetao Irrigation District in China were used to parameterize the HYDRUS-1D numerical model. The study area was spatially discretized into 18,000 compartments (30 m × 30 m × 0.02 m), and Monte Carlo simulations were applied to generate 2000 different soil-particle size distributions
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Makaravičiūtė, Lygita, and Eglė Marčiulaitienė. "CONDUCTIVITY TESTING AND EVALUATION / PAVIRŠINIŲ NUOTEKŲ FILTRO HIDRAULINIO LAIDUMO TYRIMAI IR VERTINIMAS." Mokslas – Lietuvos ateitis 7, no. 4 (2015): 436–42. http://dx.doi.org/10.3846/mla.2015.810.

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Surface wastewater is consideredas effluents, which are formed on the surface of urbanized areas. Stormwater treatment is performed out using a variety of filters: sand, grass. Wastewater penetration into the deeper layers is called hydraulic conductivity. After evaluation of the hydraulic conductivity, it is possible to determine the ability of the investigated fillers to entrap the stormwater flow. The hydraulic conductivity tests can indicate which fillers of stormwater filters may influence the more effective stormwater cleaning. Four stormwater filters were tested: crushed autoclaved aera
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Kim, Jeong Jik, Woo-Hyun Jeon, and Jin-Yong Lee. "Estimation of deep percolation using field moisture observations and HYDRUS-1D modeling in Haean basin." Journal of the Geological Society of Korea 54, no. 5 (2018): 545–56. http://dx.doi.org/10.14770/jgsk.2018.54.5.545.

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Leterme, B., D. Mallants, and D. Jacques. "Sensitivity of groundwater recharge using climatic analogues and HYDRUS-1D." Hydrology and Earth System Sciences 16, no. 8 (2012): 2485–97. http://dx.doi.org/10.5194/hess-16-2485-2012.

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Abstract. The sensitivity of groundwater recharge to different climate conditions was simulated using the approach of climatic analogue stations, i.e. stations presently experiencing climatic conditions corresponding to a possible future climate state. The study was conducted in the context of a safety assessment of a future near-surface disposal facility for low and intermediate level short-lived radioactive waste in Belgium; this includes estimation of groundwater recharge for the next millennia. Groundwater recharge was simulated using the Richards based soil water balance model HYDRUS-1D a
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Meng, Yingying, Huixiao Wang, Jiangang Chen, and Shuhan Zhang. "Modelling Hydrology of a Single Bioretention System with HYDRUS-1D." Scientific World Journal 2014 (2014): 1–10. http://dx.doi.org/10.1155/2014/521047.

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A study was carried out on the effectiveness of bioretention systems to abate stormwater using computer simulation. The hydrologic performance was simulated for two bioretention cells using HYDRUS-1D, and the simulation results were verified by field data of nearly four years. Using the validated model, the optimization of design parameters of rainfall return period, filter media depth and type, and surface area was discussed. And the annual hydrologic performance of bioretention systems was further analyzed under the optimized parameters. The study reveals that bioretention systems with under
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Chen, Min, Garry R. Willgoose, and Patricia M. Saco. "Spatial prediction of temporal soil moisture dynamics using HYDRUS-1D." Hydrological Processes 28, no. 2 (2012): 171–85. http://dx.doi.org/10.1002/hyp.9518.

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LIU, Chun-lei, Hui-feng YANG, and Gui-ling WANG. "Back calculation of soil hydraulic parameters based on HYDRUS-1D." Journal of Groundwater Science and Engineering 2, no. 3 (2014): 46–53. http://dx.doi.org/10.26599/jgse.2014.9280030.

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41

Ventrella, Domenico, Mirko Castellini, Simone Di Prima, Pasquale Garofalo, and Laurent Lassabatère. "Assessment of the Physically-Based Hydrus-1D Model for Simulating the Water Fluxes of a Mediterranean Cropping System." Water 11, no. 8 (2019): 1657. http://dx.doi.org/10.3390/w11081657.

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In a context characterized by a scarcity of water resources and a need for agriculture to cope the increase of food demand, it is of fundamental importance to increase the water use efficiency of cropping systems. This objective can be meet using several currently available software packages simulating water movements in the “soil–plant–atmosphere” continuum (SPAC). The goal of the paper is to discuss and optimize the strategy for implementing an effective simulation framework in order to describe the main soil water fluxes of a typical horticultural cropping system in Southern Italy based on
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Silva, Jeff Allen Kai, Jiří Šimůnek, and John E. McCray. "A Modified HYDRUS Model for Simulating PFAS Transport in the Vadose Zone." Water 12, no. 10 (2020): 2758. http://dx.doi.org/10.3390/w12102758.

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The HYDRUS unsaturated flow and transport model was modified to simulate the effects of non-linear air-water interfacial (AWI) adsorption, solution surface tension-induced flow, and variable solution viscosity on the unsaturated transport of per- and polyfluoroalkyl substances (PFAS) within the vadose zone. These modifications were made and completed between March 2019 and May 2019, and were implemented into both the one-dimensional (1D) and two-dimensional (2D) versions of HYDRUS. Herein, the model modifications are described and validated against the available literature-derived PFAS transpo
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Pinho, Roque E. da C. de, and Jarbas H. de Miranda. "Avaliação do modelo HYDRUS-1D na simulação do transporte de água e potássio em colunas preenchidas com solos tropicais." Engenharia Agrícola 34, no. 5 (2014): 899–911. http://dx.doi.org/10.1590/s0100-69162014000500009.

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A preocupação com o destino de produtos químicos e água, aplicados ao solo, tem motivado vários pesquisadores a desenvolverem e aplicarem modelos teóricos, a fim de descrever os processos físicos envolvidos no transporte desses produtos no perfil do solo. Nesse sentido, esta pesquisa teve como objetivo aplicar o modelo HYDRUS-1D, bem como avaliar sua performance, em simulações do deslocamento do potássio e água (umidade do solo), em colunas segmentadas, preenchidas com dois tipos de solos tropicais, em condições não saturadas (Latossolo Vermelho- - Amarelo e Nitossolo Vermelho). Os parâmetros
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Sándor, Renáta, and Nándor Fodor. "Simulation of Soil Temperature Dynamics with Models Using Different Concepts." Scientific World Journal 2012 (2012): 1–8. http://dx.doi.org/10.1100/2012/590287.

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This paper presents two soil temperature models with empirical and mechanistic concepts. At the test site (calcaric arenosol), meteorological parameters as well as soil moisture content and temperature at 5 different depths were measured in an experiment with 8 parcels realizing the combinations of the fertilized, nonfertilized, irrigated, nonirrigated treatments in two replicates. Leaf area dynamics was also monitored. Soil temperature was calculated with the original and a modified version of CERES as well as with the HYDRUS-1D model. The simulated soil temperature values were compared to th
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Klement, Aleš, Miroslav Fér, Šárka Novotná, Antonín Nikodem, and Radka Kodešová. "Root distributions in a laboratory box evaluated using two different techniques (gravimetric and image processing) and their impact on root water uptake simulated with HYDRUS." Journal of Hydrology and Hydromechanics 64, no. 2 (2016): 196–208. http://dx.doi.org/10.1515/johh-2016-0016.

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Abstract Knowledge of the distribution of plant roots in a soil profile (i.e. root density) is needed when simulating root water uptake from soil. Therefore, this study focused on evaluating barley and wheat root densities in a sand-vermiculite substrate. Barley and wheat were planted in a flat laboratory box under greenhouse conditions. The box was always divided into two parts, where a single plant row and rows cross section (respectively) was simulated. Roots were excavated at the end of the experiment and root densities were assessed using root zone image processing and by weighing. For th
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Nichols, William, Andrea Welker, Robert Traver, and Min-cheng “Peter” Tu. "Modeling Seasonal Performance of Operational Urban Rain Garden Using HYDRUS-1D." Journal of Sustainable Water in the Built Environment 7, no. 3 (2021): 04021005. http://dx.doi.org/10.1061/jswbay.0000941.

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Stafford, Madison J., Hartmut M. Holländer, and Karen Dow. "Estimating groundwater recharge in the assiniboine delta aquifer using HYDRUS-1D." Agricultural Water Management 267 (June 2022): 107514. http://dx.doi.org/10.1016/j.agwat.2022.107514.

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48

Leterme, B., D. Mallants, and D. Jacques. "Estimation of future groundwater recharge using climatic analogues and Hydrus-1D." Hydrology and Earth System Sciences Discussions 9, no. 1 (2012): 1389–410. http://dx.doi.org/10.5194/hessd-9-1389-2012.

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Abstract. The impact of climate change on groundwater recharge is simulated using climatic analogue stations, i.e. stations presently under climatic conditions corresponding to a given climate state. The study was conducted in the context of a safety assessment of a future near-surface disposal facility for low and intermediate level short-lived radioactive waste in Belgium; this includes estimating groundwater recharge for the next millennia. Groundwater recharge was simulated using the Richard's based soil water balance model Hydrus-1D and meteorological time series from analogue stations. W
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Chavoshi, E., M. Afyuni, and M. A. Hajabbasi. "Simulation of Fluoride Transport in a Calcareous Soil Using HYDRUS-1D." Journal of Water and Soil Science 19, no. 72 (2015): 205–16. http://dx.doi.org/10.18869/acadpub.jstnar.19.72.18.

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Elmi, Abdirashid, Joumana S. Abou Nohra, Chandra A. Madramootoo, and William Hendershot. "Estimating phosphorus leachability in reconstructed soil columns using HYDRUS-1D model." Environmental Earth Sciences 65, no. 6 (2011): 1751–58. http://dx.doi.org/10.1007/s12665-011-1154-1.

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