Modeling of hydrological processes in arid agricultural regions

doi:10.15302/J-FASE-2015076

Front. Agr. Sci. Eng.

2015, Vol. 2

Issue (4) : 283-294 https://doi.org/10.15302/J-FASE-2015076

REVIEW

Modeling of hydrological processes in arid agricultural regions

Jiang LI¹,Xiaomin MAO^1,^*(

),Shaozhong KANG¹,David A. BARRY²

1. College of Water Resources and Civil Engineering, China Agricultural University, Beijing 100083, China
2. Laboratoire de technologie écologique, Institut d’ingénierie de l’environnement, Station 2, Ecole polytechnique fédérale de Lausanne (EPFL), CH-1015 Lausanne, Switzerland

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Abstract

Understanding of hydrological processes, including consideration of interactions between vegetation growth and water transfer in the root zone, underpins efficient use of water resources in arid-zone agriculture. Water transfers take place in the soil-plant-atmosphere continuum, and include groundwater dynamics, unsaturated zone flow, evaporation/transpiration from vegetated/bare soil and surface water, agricultural canal/surface water flow and seepage, and well pumping. Models can be categorized into three classes: (1) regional distributed hydrological models with various land uses, (2) groundwater-soil-plant-atmosphere continuum models that neglect lateral water fluxes, and (3) coupled models with groundwater flow and unsaturated zone water dynamics. This review highlights, in addition, future research challenges in modeling arid-zone agricultural systems, e.g., to effectively assimilate data from remote sensing, and to fully reflect climate change effects at various model scales.

Keywords hydrological processes irrigation area SPAC crop growth groundwater canal seepage

Corresponding Author(s): Xiaomin MAO

Just Accepted Date: 04 December 2015 Online First Date: 28 December 2015 Issue Date: 19 January 2016

Cite this article:

Jiang LI,Xiaomin MAO,Shaozhong KANG, et al. Modeling of hydrological processes in arid agricultural regions[J]. Front. Agr. Sci. Eng. , 2015, 2(4): 283-294.

URL:

https://academic.hep.com.cn/fase/EN/10.15302/J-FASE-2015076
https://academic.hep.com.cn/fase/EN/Y2015/V2/I4/283

Fig.1 Main hydrological processes in arid areas

Tab.1 Comparison of attributes of different hydrological models

Fig.2 Conceptual depiction of a regional distributed hydrological model (modified from Beven et al.^[85^])

Fig.3 Overview of the GSPAC model

Fig.4 Overview of a coupled vadose zone-groundwater flow model. q is the volumetric soil water content; h is the soil pressure head; x, y, z are the coordinate symbols; t is time; K is the soil hydraulic conductivity; S and W are the source/sink terms; K_x, K_y and K_z are the hydraulic conductivity in directions x, y and z; m_s is the specific yield and S_s is the elastic drainable porosity.

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