Impact of Water Allocation on Soil Desalination and Groundwater Hydro-chemical Characteristics: A Temporal and Spatial Analysis of a Case Study Region in China

被引:0
|
作者
Li, P. [1 ]
Magzum, N. [2 ]
Qi, X. [1 ]
Zhang, Y. [3 ]
Du, Z. [2 ]
Liang, Z. [2 ]
Huang, Z. [3 ]
机构
[1] Chinese Acad Agr Sci, Farmland Irrigat Res Inst, Xinxiang, Henan, Peoples R China
[2] Chinese Acad Agr Sci, Agr Water & Soil Environm Field Sci Res Stn Xinxi, Xinxiang, Henan, Peoples R China
[3] Chinese Acad Agr Sci, Key Lab High Efficient & Safe Utilizat Agr Water, Xinxiang, Henan, Peoples R China
关键词
Combined well canal irrigation; Water allocation; Soil salinity; Desalinization rate; Hydro-chemical characteristics; Sodium adsorption ratio; HUAI-HAI PLAIN; SUMMER MAIZE; IRRIGATION; SALINITY; QUALITY; SALINIZATION; LAND;
D O I
10.24850/j-tyca-2019-04-11
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The influence of water resources allocation patterns on root layers soil desalination and groundwater quality were investigated by monitoring different irrigation area from People's Victory Canal irrigation district in Huang Huai Hai plain China that had been conducted well canal combined irrigation patterns from 1954. A typical area was chosen belong to the People's Victory Canal irrigation district from 2013 to 2015. Precipitation of the area, surface water irrigation amount, groundwater consumption amount, salinity content in 0 to 100 cm soil layer and total dissolved solids in groundwater were monitored, the ratio of canal-well water (the ratio of surface water to groundwater irrigation amount, CWWR), soil salinity spatial dynamic, desalinization rate in 0 to 100 cm soil layer and sodium adsorption ratio (SAR) of groundwater were analyzed in the area. CWWR of Branch 1, Branch 2, and Branch 3 ranged from 0.72 to 1.03, 2.50 to 2.63, and 0.65 to 1.26 in 2013 to 2015, respectively. The soil salinity contents for the top 100 cm horizons in the Branch 2 irrigation area decreased slightly by 1.63% to 8.90% compared with the values in the Branch 1 and Branch 3 irrigation districts while the water resources allocation patterns were conducted two years later. Compared with the area in the hydrological period in 2013, the area of average soil salinity exceeded 0.32 mS/cm for the top 20 cm horizons has decreased notably in 2014 and 2015. Compared with the values in 2014, the average TDS concentration of groundwater increased by 18.66% in the study area in 2015, whereas the sodium adsorption ratio (SAR) values in the above-mentioned irrigation areas decreased by 23.58%, 36.82%, and 53.37% in the normal period in 2015. The combined well-canal irrigation pattern could represent a useful water allocation method mainly because of the temporal and spatial regulation of water resources and root layer soil desalination; however, possible increases of TDS in the groundwater may cause potential ecosystem degradation risks after long-term water allocation in semi-arid areas. Thus, water allocation should be emphasized to maintain a healthy groundwater environment and sustainable stable yields of grain in combined canal-well irrigation districts.
引用
收藏
页码:219 / 237
页数:19
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