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松辽平原区域水文地质特征与水资源及其开发战略 被引量:3

REGIONAL HYDROGEOLOGICAL FEATURES AND WATER RESOURCES OF THE SONGLIAO PLAIN AND ITS DEVELOPING STRATEGY
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摘要 松辽平原的水资源问题,已成为我国东北地区各项经济建设发展的制约因素,日益为人们所关注。在综合前人资料的基础上,本文对松辽平原区域地下水形成分布特点及水资源状况进行了系统的分析,同时还提出了一些水资源开发战略措施,供有关部门制定国民经济和社会发展规划时参考。 The Songliao plain is originally basin-type plain formed in the tectonic framework of Subsidence zone No.2 of Neocathaysian tectonic system.it dominates the recharge,runoff,storage and discharge condition of ground- water,with the characteristics of basin-type lateral zoning in the basic framework of the groundwater system. The Songnen plain is an asymmetric groundwater basin.The exploitable amount of undergroundwater is 137.37×10~8m^3/a,surfaee flow,65.20×10~3m^3/a, and surface outflow,438.69×10~3m^3/a.The Shangliaohe plain is an un-uniform groundwater basin.The distribution of groundwater in the Zhongliaohe plain indicates un-uniformity,and the exploitable groundwater resources,61.25× 10~3m^3/a,surfce flow,21.18×10~3m^3/a,surface cutflow,40.16×10~8m^3/a.The Xia- liaohe plain is a groundwater basin with symmetric zoning open to south,and the exploitable groundwater resources,46.79×10~3m^3/a,surface flow,22.20×10~8 m^3/a,surface inflow,116.38×10~8m^3/a. The utilized amount of groundwater occupied 20.26% of the exploitable groundwater resources,and the utilized amount of surface water occupied 27.99% of the total amount of surface flow,indicating that the water resour- ces of the Songliao plain is potential in development.Because the water resources is not distributed uniformly and exploited excessively or irrationally, the water is in short supply. The key to solve the deficiency in water resources of the Songliao plain is formulation and implementation of feasible development strategy.The strate- gies include:Based upon the different conditions of water resources,exploit- ing water resources rationally;establishing the water saving production system of industry and agriculture;utilizing the water resources scientifically;carry- ing out the joint exploitation of surface and undergroundwater and man-made store water and management;increasing more new water sources;establishing united,long-term monitoring system of all water sources;protecting water sources;and managing water resources according to the state law and econom- ic policies.
作者 张勃夫
出处 《吉林地质》 1989年第3期1-9,共9页 Jilin Geology
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  • 1张勃夫.长白山区地下水资源评价与合理利用[J].自然资源学报,1987,2(4):321-336. 被引量:6
  • 2裘善文.松辽平原低涝易洼的.盐碱地综合治理与农业发展[M].北京:科学出版社,1996.1-7.
  • 3张勃夫.吉林省水文地质工作进展[J].地质科技通报,1982,(10).
  • 4张勃夫.吉林省地下水资源及开发前景[J].吉林地质,1988,(3).
  • 5张勃夫 刘祯 等.吉林省地质环境治理保护战略对策研究.吉林省减灾论文集[M].吉林科技出版社,1992..
  • 6张勃夫 张振权.吉林省地下水资源开发利用.中国地下水资源开发利用[M].内蒙古人民出版社,1992..
  • 7王风生.吉林省地下水[M].长春:吉林科技出版社,1998..
  • 8裘善文,松嫩平原盐碱地与风沙地农业综合发展研究,1997年,917页
  • 9裘善文,松辽平原低涝易洼,盐碱地综合治理与农业发展,1996年,17页
  • 10张勃夫,吉林地质,1989年,3卷,19页

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