地理学

制约济南岩溶大泉持续喷涌的主因素阈值研究

  • 周娟 ,
  • 邢立亭 ,
  • 滕朝霞 ,
  • 王立艳
展开
  • 1. 济南大学 资源与环境学院,济南250022; 
    2. 山东省地下水数值模拟及污染控制工程技术中心,济南250022;
    3. 济南市水利局,济南250099
周娟,女,硕士研究生. 主要研究方向为地下水资源与数值模拟.

收稿日期: 2014-04-07

  网络出版日期: 2015-05-28

基金资助

国家自然科学基金(41172222);济南市科技发展计划项目(201303082)

Study on the threshold of main factors restricting Jinan large karst springs spewing

  • ZHOU Juan ,
  • XING Li-Ting ,
  • TENG Chao-Xia ,
  • WANG Li-Yan
Expand

Received date: 2014-04-07

  Online published: 2015-05-28

摘要

为保护济南泉水,实施了减采和回灌措施,回归分析计算表明,1972—2002年泉水断流期间影响泉水位的主要因素是开采量,2003年以来泉水持续喷涌阶段开采量降至次要因素.基于2004—2012年间泉水位动态观测资料,采用地下水位动态线型特征系数法确定济南的岩溶裂隙发育较好;运用SPSS软件对降雨、回灌两个因子对泉水位影响程度进行分析,建立泉水位与月降雨回归—自回归模型,结果显示前一个月降雨对泉水位具有显著性影响;建立泉水位与降水量高次趋势模型,计算枯水期维持济南泉水动态稳定的月降雨阈值为26.65~30.73 mm;基于人工回灌量与泉水水位分析,计算得出枯水期保泉回灌补源量应不小于16.56万m3/d.研究结果表明,泉水位受气象和人为影响较敏感,为济南保泉与地下水回灌补源提供科学依据.

本文引用格式

周娟 , 邢立亭 , 滕朝霞 , 王立艳 . 制约济南岩溶大泉持续喷涌的主因素阈值研究[J]. 华东师范大学学报(自然科学版), 2015 , 2015(3) : 146 . DOI: 10.3969/j.issn.1000-5641.2015.03.017

Abstract

Jinan spring groups are famous large karst springs in north China. The interaction of natural factors and human impact had caused a decline in jinan karstic water level. Jinan spring groups began to appear cutoff in 1972, and the cutoff lasted from 1972 to 2002. To protect the jinan springs, some measures, like reducing groundwater exploitation and artificial recharge have been carried out. The result of regression analysis shows that, during that cutoff period, the main reason affecting spring water level is groundwater exploitation, but since 2003, Jinan spring groups have resumed spewing, and groundwater exploitation is no longer a major factor affecting the spring water level. Based on the series dynamic observation data of Jinan springs water level from 2004 to 2012, it is determined that the development degree of Jinan karst is relatively high by the method of dynamic characteristics curve types of karst water level. Through SPSS software, the influence degree on springs water level caused by precipitation and artificial recharge was analyzed. The regression—autoregressive model was built, which shows that the last month precipitation has significant effect on the water level. Using the higher order trend mathematical model about springs water level and precipitation, it is calculated that the monthly precipitation threshold is 26.65~30.73 mm to maintain Jinan spring dynamic stability in dry season. Finally, for spring protection, the paper puts forward that the artificial recharge water quantity is not less than 165 600 m3/d in dry season. Research suggests that springs water level is sensitive to climate change and human activities, and our research results can provide some scientific basis for the jinan springs protection and groundwater recharge. 

参考文献

[1]王维泰,梁永平,王占辉,等.中国北方气候变化特征及其对岩溶水的影响[J].水文地质工程地质,2012,39(6):610.

[2]FAN Y H, HUO X L, HAO Y H, et al. An assembled extreme value statistical model of karst spring discharge[J]. Journal of Hydrology,2013,504(11):5768.

[3]袁道先.中国岩溶学[M].北京:地质出版社,1993:18.

[4]ELLEN K H, LAURA T, WILLIAM B W. Quantifying the place of karst aquifers in the groundwater to surface water continuum: A time series analysis study of storm behavior in Pennsylvania water resources[J].Journal of Hydrology,2009,376:307317.

[5]王大纯.水文地质学基础[M].北京:地质出版社,1995:100101.

[6]陈葆仁,洪再吉,汪福炘,等.地下水动态及其预测[M].北京:科学出版社,1988.

[7]张建芝.济南泉域地下水动态特征及监测网优化[D].济南:济南大学,2011.

[8]张建芝,邢立亭.回归分析法在地下水动态分析中的应用[J].地下水,2010,32(4):8890.

[9]JAN C D, CHEN T H, HUANG H M. Analysis of rainfallinduced quick groundwaterlevel response by using a Kernel function[J].Paddy Water Environment, 2013(11):135144.

[10]胡克祯,张建芝,邢立亭.基于时间序列分析的地下水动态研究[J].水科学与工程技术,2011(5):3234.

[11]MAO X M, SHANG S H, LIU X. Groundwater level predictions using artificial neural networks[J].Tsinghua Science and Technology,2002,7(6):574579.

[12]吴东杰,王金生,滕彦国.小波分解与变换法预测地下水位动态[J].水利学报,2004,(5):4944.

[13]DAMIR J, VESNA D J. A frequency domain approach to groundwater recharge estimation in karst[J].Journal of Hydrology,2004,289:95110.

[14]祁晓凡,杨丽芝,韩晔.济南泉域地下水位动态及其对降雨响应的交叉小波分析[J].地球科学进展,2012,27(9):970978.

[15]王茂枚,束龙仓,季叶飞,等.济南岩溶泉水流量衰减原因分析及动态模拟[J].中国岩溶,2008,27(1):1923.

[16]邢立亭.济南泉域岩溶水环境保护[J].水利科技与经济,2006,12(9):601604.

[17]吴兴波,牛景涛,牛景霞,等.人工回灌对济南泉水系统修复的影响[J].人民黄河,2004,26(8):2022.

[18]牛景涛,吴兴波,宋星原,等.济南回灌补源与抽水试验研究[J].人民长江,2004,35(11):4748.

[19]章亦兵.济南市人工回灌补源保护泉水的研究[D].南京:河海大学,2005.

[20]徐军祥,邢立亭,魏鲁峰,等.济南岩溶水系统研究[M].北京:冶金工业出版社,2012:2635.

[21]邹成杰.岩溶地区地下水位动态分析[J].中国岩溶,1995,14(3):261269.

[22]李传谟,康凤新.山东羊庄岩溶水系统水资源及增源增采最佳开发研究[G]//山东省地质矿产局主编.山东地质矿产研究文集.济南:山东科学技术出版社,1996:224227.

[23]李传谟,康凤新.岩溶水资源及增采模型[M].济南:山东科学技术出版社,1999:5156.
文章导航

/