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Fatemeh Gheybi, Parivash Paridad, Farid Faridani, Ali Farid, Alonso Pizarro, Mauro Fiorentino and Salvatore Manfreda
Monitoring Surface Soil Moisture (SSM) and Root Zone Soil Moisture (RZSM) dynamics at the regional scale is of fundamental importance to many hydrological and ecological studies. This need becomes even more critical in arid and semi-arid regions, where t...
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Yonghao Liu, Taohui Li, Wenxiang Zhang and Aifeng Lv
Root-zone soil moisture (RZSM) plays a key role in the hydrologic cycle and regulates water?heat exchange. Although site observations can provide soil profile moisture measurements, they have a restricted representation. Satellites can determine soil moi...
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Kenneth J. Tobin and Marvin E. Bennett
This study examined eight Great Plains moderate-sized (832 to 4892 km2) watersheds. The Soil and Water Assessment Tool (SWAT) autocalibration routine SUFI-2 was executed using twenty-three model parameters, from 1995 to 2015 in each basin, to identify hi...
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Valentin Gómez Sanz,J I Garcia-Viñas
Pág. 293 - 302
Pinus pinaster stands in the center of the Iberian Peninsula frequently grow in a unique hydrological system characterized by a variable groundwater table near the soil surface and highly permeable soils (arenosols). Over the last few decades, this super...
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Rong Ren, Juanjuan Ma, Qiyun Cheng, Lijian Zheng, Xianghong Guo, Xihuan Sun
Pág. 1 - 22
Temperature is an integral part of soil quality in terms of moisture content; coupling between water and heat can render a soil fertile, and plays a role in water conservation. Although it is widely recognized that both water and heat transport are funda...
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Rong Ren, Juanjuan Ma, Qiyun Cheng, Lijian Zheng, Xianghong Guo and Xihuan Sun
Temperature is an integral part of soil quality in terms of moisture content; coupling between water and heat can render a soil fertile, and plays a role in water conservation. Although it is widely recognized that both water and heat transport are funda...
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Hao Duan, Hongli Zhao, Qiuju Li, Haowei Xu and Chengxin Han
Most of the current parameterization schemes for the Penman?Monteith?Leuning evapotranspiration (ET) model (PML) consider meteorological and energy factors and land use types, but the analysis of the effect of soil moisture (SM) changes on ET processes l...
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Khaled Mohammed, Robert Leconte and Mélanie Trudel
Soil moisture modeling is necessary for many hydrometeorological and agricultural applications. One of the ways in which the modeling of soil moisture (SM) can be improved is by assimilating SM observations to update the model states. Remotely sensed SM ...
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Zebin Liu, Yanhui Wang, Pengtao Yu, Ao Tian, Yarui Wang, Wei Xiong and Lihong Xu
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Yongchul Shin, Kyoung Jae Lim, Kyungwon Park, Younghun Jung
Pág. 1 - 15
Several inversion modeling-based approaches have been developed/used to extract soil hydraulic properties (a, n, ?res, ?sat, Ksat) from remotely sensed (RS) soil moisture footprints. Hydrological models with shallow ground water (SGW) table depths in soi...
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Yongchul Shin, Kyoung Jae Lim, Kyungwon Park and Younghun Jung
Several inversion modeling-based approaches have been developed/used to extract soil hydraulic properties (a, n, ?res, ?sat, Ksat) from remotely sensed (RS) soil moisture footprints. Hydrological models with shallow ground water (SGW) table depths in soi...
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Chitao Sun, Di Feng, Zhaorong Mi, Caixia Li, Junpeng Zhang, Yang Gao and Jingsheng Sun
Flat (F), mini-ditch (MD), and ridge-furrow (RF) are three conventional cotton planting patterns that are usually adopted around the world, yet soil and crop responses to these three patterns are poorly studied, as is their suitability for increasing yie...
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Chitao Sun, Di Feng, Zhaorong Mi, Caixia Li, Junpeng Zhang, Yang Gao, Jingsheng Sun
Pág. 1 - 15
Flat (F), mini-ditch (MD), and ridge-furrow (RF) are three conventional cotton planting patterns that are usually adopted around the world, yet soil and crop responses to these three patterns are poorly studied, as is their suitability for increasing yie...
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Christos Tzimopoulos, Nikiforos Samarinas, Basil Papadopoulos and Christos Evangelides
The process of how soil moisture profiles evolve into the soil and reach the root zone could be estimated by solving the appropriate strong nonlinear Richards? equation. The nonlinearity of the equation occurs because diffusivity D is generally an expone...
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Nils Siering and Helmut Grüning
Stormwater tree pits with storage elements enable the irrigation of urban trees and can potentially act as decentralized rainwater retention basins. This paper mainly focuses on analyzing this potential. Field tests were conducted to investigate the irri...
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Florin Nenciu, Marius Remus Oprescu and Sorin-Stefan Biris
Water is the primary limiting factor in dryland crop production, therefore emerging approaches for preserving rainwater to be more accessible to plants, for extended periods of time, can significantly improve agricultural system efficiency. Furrow diking...
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Peirong Lu, Zhanyu Zhang, Genxiang Feng, Mingyi Huang and Xufan Shi
Initial land reclamation of the saline soils often requires higher drainage intensity for quick leaching of salts from the soil profile; however, drainage pipes placed at closer spacing may result in higher cost. Seeking an inexpensive degradable organic...
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Inken Rabbel, Heye Bogena, Burkhard Neuwirth and Bernd Diekkrüger
Tree water use is a key variable in forest eco-hydrological studies and is often monitored by sap flow measurements. Upscaling these point measurements to the stand or catchment level, however, is still challenging. Due to the spatio-temporal heterogenei...
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Inken Rabbel, Heye Bogena, Burkhard Neuwirth and Bernd Diekkrüger
Tree water use is a key variable in forest eco-hydrological studies and is often monitored by sap flow measurements. Upscaling these point measurements to the stand or catchment level, however, is still challenging. Due to the spatio-temporal heterogenei...
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Thomas K. Alexandridis, Ines Cherif, George Bilas, Waldenio G. Almeida, Isnaeni M. Hartanto,
Pág. 1 - 16
Despite playing a critical role in the division of precipitation between runoff and infiltration, soil moisture (SM) is difficult to estimate at the catchment scale and at frequent time steps, as is required by many hydrological, erosion and flood simula...
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