|
|
|
| Exploitation and utilization of groundwater and potential water source analysis of Fengpei Plain area |
| JING Jiajun1, GUAN Zhen1, SHAN Yuyang1, JING Jiayuan2 |
1. No.5 Geological Team of Jiangsu Geology and Mineral Bureau, Xuzhou 221004, China;
2. North China University of Science and Technology, Tangshan 063600, China |
|
|
|
|
Abstract By summarizing hydrogeological conditions and characteristics of Fengpei Plain area, the authors has analyzed the exploitation and utilization conditions of groundwater and potential water source. And the available resources of karst water in Huaqi uplift were calculated and the feasibility of karst water utilization was discussed. The results show that the main groundwater level in the study area is middle and upper Pleistocene pore aquifer and Neogene-Lower Pleistocene pore aquifer, which have already formed two super large funnel areas of Chengguan of Fengxian-Sunlou-Changdian and Peixian-Longgu, with the total area exceeding 750 km2 , causing large ground subsidence area. Huaqi uplift is the karst water-rich area, with the total recoverable resources of 667.51×104 m3/a. This area can be regarded as potential water source area for further groundwater exploitation. Excess exploitation of karst water can cause problems such as land subsidence, karst ground collapse, so long-term monitoring of karst water exploitation in the future and reasonable usage of groundwater are necessary. The karst water in Huaqi uplift is close to the urban area with large volume and good quality, and it is relatively easy to develop, which means it has considerable economic value.
|
|
Received: 24 May 2018
|
|
|
|
|
|
[1] 黄晓燕,冯志祥,李朗,等.江苏省地下水超采区划分方法对比研究[J].水文地质工程地质,2014,41(6):26-31.
[2] 孟磊,冯启言,张海荣,等.徐州大屯中心区地面沉降机理分析与危险性评价[J].中国地质灾害与防治学报,2008,19(3):60-63.
[3] 景佳俊,陶文杰,管祯.徐州市第四系孔隙水特征研究[J].中国地质调查,2017,4(2):73-77.
[4] 张阿根,刘毅,龚士良.国际地面沉降研究综述[J].上海地质,2000(4):1-7.
[5] 陈崇希. 关于地下水开采引发地面沉降灾害的思考[J].水文地质工程地质,2000,27(1):45-48,60.
[6] 杨林权. 荷载和地下水开采作用下的地面沉降数值模拟及应用研究[D].武汉:中国地质大学(武汉),2014.
[7] 花修权,黄敬军,缪世贤,等.徐州市地质灾害分布特征及成因分析[J].地质灾害与环境保护,2015,26(2):74-80.
[8] 景佳俊,陶文杰,管祯.对江苏沛县新庄铁矿区富水性规律的初步认识[J].中国地质调查,2016,3(6):68-74.
[9] 周贤金,乔祥云.姜梨园铁矿区矿坑涌水量预测模拟[J].矿产勘查,2011,2(3):311-315.
[10] 潘万乾,王文庆,陆华,等.江苏省沛县封新庄矿区铁矿详查地质报告[R].南京:江苏省地质调查研究院,2006:35-47.
[11] 中国地质调查局.水文地质手册[M].2版.北京:地质出版社,2012:690-693. |
| [1] |
YAN Xuexin, WANG Hanmei, YANG Tianliang, HUANG Xinlei, ZHAN Guanghui, HE Ye. Major achievements of land subsidence caused by deep foundation pits dewatering in coastal areas and their applications: A case study of Shanghai[J]. , 2019, 6(1): 67-74. |
| [2] |
PENG Peng, YANG Honglei. Study of land subsidence monitoring based on an improved coherent point target technology in Fuyang City[J]. , 2016, 3(4): 63-68. |
| [3] |
ZHOU Dan, XING Xue, WANG Hongpei. Stability analysis and evaluation of land subsidence in Suiningurban area of Xuzhou City, Jiangsu Province[J]. , 2016, 3(1): 58-64. |
| [4] |
ZHANG Jin-cai, CHU Li-feng, XIAO Zhen, LU Ze-chang, SHEN Rong-hui, CHEN Ying-jie. Main Progress and Achievements of Land Subsidence Survey and Monitoring in Hebei Plain[J]. , 2014, 1(2): 45-50. |
|
|
|
|
2019, Vol. 6 
