黑龙江中下游中俄跨国界含水层俄罗斯侧区域特征分析
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摘要
以黑龙江中下游中俄跨国界含水层俄罗斯侧作为研究区,并以黑龙江流域为背景,对该流域位置与范围进行综述,根据地质结构、岩石性质等因素把黑龙江流域分成9个水文地质分区。其中,黑龙江流域有3个中俄跨国界含水层,研究区所在的水文地质单元为黑龙江中下游中俄跨国界含水层,它位于黑龙江流域9个水文地质分区的"三江平原海洋气候带水文地质区"。该含水层分为中国侧和俄罗斯侧,可从行政区划、地表水区划、地下水区划3个因素对其进行特征分析,最后分析了研究区与其所在的水文地质单元中国侧之间的关联。对黑龙江中下游中俄跨国界含水层俄罗斯侧进行区域特征分析,将有助于今后对其进行地下水与地表水交换方面的研究,并对其他地区典型跨国界含水层区域特征分析提供思路参考和方法借鉴。
Taking the Russian side of Sino-Russian transboundary aquifer in the middle and lower reaches of Heilongjiang River as the research area, and taking the Heilongjiang River Basin as the background, this paper summarizes the location and scope of the basin, and divides the Heilongjiang River Basin into nine hydrogeological zones according to geological structure, rock properties and other factors. Among them, there are three Sino-Russian transboundary aquifers in Heilongjiang River Basin. The hydrogeological unit of the research area is the Sino-Russian transboundary aquifer in the middle and lower reaches of Heilongjiang River which is located in the "Hydrogeological Area of Marine Climate Zone in Sanjiang Plain" of nine hydrogeological zones in Heilongjiang River Basin. The aquifer is divided into the Chinese side and the Russian side, and it can be analyzed from three factors: administrative division, surface water division and groundwater division. Finally, the relationship between the research area and the other side of its hydrogeological unit is analyzed. The regional characteristics analysis on Russian side of Sino-Russian transboundary aquifers in the middle and lower reaches of Heilongjiang(Amur) River will be helpful to the study of groundwater and surface water exchange in the future, and provides ideas and methods for the analysis of regional characteristics of typical transboundary aquifers in other regions.
Taking the Russian side of Sino-Russian transboundary aquifer in the middle and lower reaches of Heilongjiang River as the research area, and taking the Heilongjiang River Basin as the background, this paper summarizes the location and scope of the basin, and divides the Heilongjiang River Basin into nine hydrogeological zones according to geological structure, rock properties and other factors. Among them, there are three Sino-Russian transboundary aquifers in Heilongjiang River Basin. The hydrogeological unit of the research area is the Sino-Russian transboundary aquifer in the middle and lower reaches of Heilongjiang River which is located in the "Hydrogeological Area of Marine Climate Zone in Sanjiang Plain" of nine hydrogeological zones in Heilongjiang River Basin. The aquifer is divided into the Chinese side and the Russian side, and it can be analyzed from three factors: administrative division, surface water division and groundwater division. Finally, the relationship between the research area and the other side of its hydrogeological unit is analyzed. The regional characteristics analysis on Russian side of Sino-Russian transboundary aquifers in the middle and lower reaches of Heilongjiang(Amur) River will be helpful to the study of groundwater and surface water exchange in the future, and provides ideas and methods for the analysis of regional characteristics of typical transboundary aquifers in other regions.
引文
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[4] 常龙艳,李文文,戴长雷,等.黑龙江(阿穆尔河)流域水文地质区划分析与探讨[J].水资源研究,2012,1(1):398-401.
[5] 韩再生,李尧,王皓,等.跨界含水层研究——世界进展和亚洲实践[J].科技导报,2012,30(5):57-66.
[6] 亚洲地质图编图组.亚洲地质图[M].北京:地质出版社,1982.
[7] 张宗祜.亚洲水文地质图[M].北京:地质出版社,1997.
[8] 唐蕴,唐克旺,康伟,等.跨界含水层研究现状与展望[J].水文地质工程地质,2010,37(5):15-19.
[9] 韩再生,王皓.跨边界含水层问题研究[J].水文地质工程地质,2006(5),80-84
[10] 韩振新.黑龙江省水文地质志[M].哈尔滨:黑龙江人民出版社,2000.
[11] 王思聪,戴长雷,赵惠媛,等.黑龙江中下游中俄跨国界含水层研究综述[J].黑龙江水利,2016,2(6):33-37.
[12] 《中国河湖大典》编纂委员会.中国河湖大典(黑龙江、辽河卷)[M].北京:中国水利水电出版社,2014.
[13] 中国地质调查局.亚洲地下水系列图[M].北京:中国地图出版社,2012.
[14] 董淑华,戴长雷,赵慧媛,等.黑龙江中下游中俄跨国界含水层水文地质图[M].哈尔滨:哈尔滨地图出版社,2017.