Arid
DOI10.3390/w7052382
Modeling of Soil Water and Salt Dynamics and Its Effects on Root Water Uptake in Heihe Arid Wetland, Gansu, China
Li, Huijie1; Yi, Jun1; Zhang, Jianguo1; Zhao, Ying1,2; Si, Bingcheng2,3; Hill, Robert Lee4; Cui, Lele1,5; Liu, Xiaoyu1
通讯作者Zhao, Ying
来源期刊WATER
ISSN2073-4441
出版年2015
卷号7期号:5页码:2382-2401
英文摘要

In the Heihe River basin, China, increased salinity and water shortages present serious threats to the sustainability of arid wetlands. It is critical to understand the interactions between soil water and salts (from saline shallow groundwater and the river) and their effects on plant growth under the influence of shallow groundwater and irrigation. In this study, the Hydrus-1D model was used in an arid wetland of the Middle Heihe River to investigate the effects of the dynamics of soil water, soil salinization, and depth to water table (DWT) as well as groundwater salinity on Chinese tamarisk root water uptake. The modeled soil water and electrical conductivity of soil solution (ECsw) are in good agreement with the observations, as indicated by RMSE values (0.031 and 0.046 cm(3)cm(-3) for soil water content, 0.037 and 0.035 dSm(-1) for ECsw, during the model calibration and validation periods, respectively). The calibrated model was used in scenario analyses considering different DWTs, salinity levels and the introduction of preseason irrigation. The results showed that (I) Chinese tamarisk root distribution was greatly affected by soil water and salt distribution in the soil profile, with about 73.8% of the roots being distributed in the 20-60 cm layer; (II) root water uptake accounted for 91.0% of the potential maximal value when water stress was considered, and for 41.6% when both water and salt stress were considered; (III) root water uptake was very sensitive to fluctuations of the water table, and was greatly reduced when the DWT was either dropped or raised 60% of the 2012 reference depth; (IV) arid wetland vegetation exhibited a high level of groundwater dependence even though shallow groundwater resulted in increased soil salinization and (V) preseason irrigation could effectively increase root water uptake by leaching salts from the root zone. We concluded that a suitable water table and groundwater salinity coupled with proper irrigation are key factors to sustainable development of arid wetlands.


英文关键词arid wetland water and salt dynamics Hydrus-1D root water uptake Chinese tamarisk
类型Article
语种英语
国家Peoples R China ; Canada ; USA
收录类别SCI-E
WOS记录号WOS:000356935900016
WOS关键词ELECTRICAL-CONDUCTIVITY ; HYDRAULIC CONDUCTIVITY ; NUMERICAL-ANALYSIS ; IRRIGATION WATER ; GROUNDWATER ; TRANSPORT ; SALINITY ; RIVER ; PRODUCTIVITY ; CALIBRATION
WOS类目Water Resources
WOS研究方向Water Resources
来源机构西北农林科技大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/190720
作者单位1.Northwest Agr & Forestry Univ, Key Lab Plant Nutr & Agrienvironm Northwest China, Minist Agr, Yangling 712100, Peoples R China;
2.Univ Saskatchewan, Dept Soil Sci, Saskatoon, SK S7N 5A8, Canada;
3.Northwest Agr & Forestry Univ, Coll Water Resources & Architecture Engn, Yangling 712100, Peoples R China;
4.Univ Maryland, Dept Environm Sci & Technol, College Pk, MD 20742 USA;
5.Minist Water Resources, Suide Test Stn Water & Soil Conservat, Yellow River Conservancy Comm, Yulin 719000, Shanxi, Peoples R China
推荐引用方式
GB/T 7714
Li, Huijie,Yi, Jun,Zhang, Jianguo,et al. Modeling of Soil Water and Salt Dynamics and Its Effects on Root Water Uptake in Heihe Arid Wetland, Gansu, China[J]. 西北农林科技大学,2015,7(5):2382-2401.
APA Li, Huijie.,Yi, Jun.,Zhang, Jianguo.,Zhao, Ying.,Si, Bingcheng.,...&Liu, Xiaoyu.(2015).Modeling of Soil Water and Salt Dynamics and Its Effects on Root Water Uptake in Heihe Arid Wetland, Gansu, China.WATER,7(5),2382-2401.
MLA Li, Huijie,et al."Modeling of Soil Water and Salt Dynamics and Its Effects on Root Water Uptake in Heihe Arid Wetland, Gansu, China".WATER 7.5(2015):2382-2401.
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