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| Analysis of effect of human activities on regional groundwater level |
| LIU Zhiyong1, LIU Dong1,2,3,4, LIU Wenting1, LUO Tianqi1 |
| 1.School of Water Conservancy & Civil Engineering, Northeast Agricultural University, Harbin, Heilongjiang 150030, China; 2.Key Laboratory of Water-Saving Agriculture of Universities in Heilongjiang Province, Northeast Agricultural University, Harbin, Heilongjiang 150030, China; 3.Collaborative Innovation Center for Improving Grain Production Capacity of Heilongjiang Province, Northeast Agricultural University, Harbin, Heilongjiang 150030, China; 4.Key Laboratory of High Efficient Utilization of Agricultural Water Resource of Ministry of Agriculture, Northeast Agricultural University, Harbin, Heilongjiang 150030, China |
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Abstract To study the effect of human activities on underground water level, taking Heilongjiang Land Reclamation Mudanjiang Administration as an example,the number of wells,crops area, groundwater irrigation area and other nine factors were chosen, as the evaluation indicators of the effect of human activities on underground water level, and the technique for order preference by similarity to ideal solution(TOPSIS)was used to establish the effect degree evaluation model for quantitative analysis of the influence of human activities on the groundwater level of each farm, which is under Mudanjiang Administration, from the year 2000 to 2013. The results show that the effect of human activities on the groundwater level of farm 855,8510,8511, Xingkai Lake, Hailin and Ning′an is minimum; that of farm 857 and Yunshan is moderate; that of farm Qingfeng and from 858 is a little higher, and that of farm 850, 854 and 856 is maximum. The results reveal the temporal and spatial differences of the human activities effect on the regional groundwater level from 2000 to 2013. In space, the effect is gradually weakened from northeast to southwest;temporally,the effect is generally enhanced from 2000 to 2003, and is gradually weakened from 2004 to 2013.
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Received: 10 November 2015
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