[1]贺晓浪,段中会,苗霖田,等.陕北毛乌素沙漠区潜水含水层富水性及动态变化特征[J].西安科技大学学报,2019,(01):88-95.[doi:10.13800/j.cnki.xakjdxxb.2019.0113 ]
 HE Xiao-lang,DUAN Zhong-hui,MIAO Lin-tian,et al.Unconfined aquifer water-richness and dynamic changefeatures of Mu Us Desert Area in northern Shaanxi[J].Journal of Xi'an University of Science and Technology,2019,(01):88-95.[doi:10.13800/j.cnki.xakjdxxb.2019.0113 ]
点击复制

陕北毛乌素沙漠区潜水含水层富水性及动态变化特征(/HTML)
分享到:

西安科技大学学报[ISSN:1672-9315/CN:61-1434/N]

卷:
期数:
2019年01期
页码:
88-95
栏目:
出版日期:
2019-02-28

文章信息/Info

Title:
Unconfined aquifer water-richness and dynamic changefeatures of Mu Us Desert Area in northern Shaanxi
文章编号:
1672-9315(2019)01-0088-08
作者:
贺晓浪12段中会3苗霖田13张建军3
(1.西安科技大学 地质与环境学院,陕西 西安 710054; 2.中煤能源研究院有限责任公司,陕西 西安 710054; 3.国土资源部煤炭资源勘查与综合利用重点实验室,陕西 西安 710021)
Author(s):
HE Xiao-lang12DUAN Zhong-hui3MIAO Lin-tian13ZHANG Jian-jun3
(College of Geology and Environment,Xi'an University of Science and Technology,Xi'an 710054,China; 2.China Coal Energy Research Institute Co.,Ltd.,Xi'an 710054,China; 3.Key Laboratory of Coal Resources Exploration and Comprehensive Utilization,Ministry of Land and Resources,Xi'an 710021,China)
关键词:
地质资源与地质工程 潜水含水层 富水性评价 保水采煤
Keywords:
geological resources and geological engineering unconfined aquifer water-richness evaluation coal mining with water protection
分类号:
TD 742.3
DOI:
10.13800/j.cnki.xakjdxxb.2019.0113
文献标志码:
A
摘要:
针对沙漠区潜水含水层富水性评价问题,基于野外调查和理论研究,总结认为毛乌素沙漠区内潜水含水层富水性主要由3层次5个因素综合控制,结合层次分析法、模糊聚类,提出了该区内潜水含水层富水性评价模型,并分析了各影响因素在一个水文年内的变化特征,综合评价了区内萨拉乌苏组潜水含水层的富水性分区特征及其动态变化规律。结果表明:区内潜水含水层以富水性弱区分布最广,且明显大于其他区域,同时该区的面积、形态也最容易受到枯水期和丰水期变化的影响。而较弱富水区的面积对季节变化不敏感,但其分布的区域发生了较大变化。相比之下,较强和强富水含水区则受到的影响较小。
Abstract:
Based on the field investigation and theoretical research,it is summarized that the water richness of phreatic aquifer in Mu Us desert area is mainly controlled by 5 factors which can be formed of 3 hierarchies,AHP(analytic hierarchy process)and fuzzy clustering method were adopted to build the water richness evaluation model of unconfined aquifer in the district,and the characteristics of each index in one hydrological year were analyzed.Partition characteristics and the dynamic change features of Salawusu phreatic aquifer were comprehensively evaluated.The results show that the area with weakest water yield is most widely distributed and significantly greater than other areas,its area and shape are also the most vulnerable to the wet and dry season change,while the area of weaker water-richness district would be less influenced by thischange,but significant changes have taken place in its distribution shape.Stronger and strongest water richness zones,in contrast,were less affected.

参考文献/References:


[1] 李文平,段中会,华解明,等.陕北榆神府矿区地质环境现状及采煤效应影响预测[J].工程地质学报,2000,8(3):324-333. LI Wen-ping,DUAN Zhong-hui,HUA Jie-ming,et al.Evaluation of present geological environment and prediction of its variation caused by mining in Yushenfu mine area of north Shaanxi[J].Journal of Engineering Geology,2000,8(3):324-333.
[2]范立民,马雄德,冀瑞君.西部生态脆弱矿区保水采煤研究与实践进展[J].煤炭学报,2015,40(8):1711-1717. FAN Li-min,MA Xiong-de,JI Rui-jun.Progress in engineering practice of water-preserved coal mining in western eco-environment frangible area[J]. Journal of China Coal Society,2015,40(8):1711-1717.
[3]Ghoubachi,Saad Younes.Impact of lake nasser on the groundwater of the Nubia sandstone aquifer system in Tushka area,South Western Desert,Egypt[J].Journal of King Saud University Science,2012 24(2):101-109.
[4]张天模,李健,施龙青,等.物探技术在矿井水防治中的应用研究[J].西安科技大学学报,2013,33(1):56-60. ZHANG Tian-mo,LI Jian,SHI Long-qing,et al.Application of geophysical exploration technique in the mine water prevention and control[J].Journal of Xi'an University of Science and Technology,2013,33(1):56-60.
[5]于师建.三软煤层上覆含水层富水性瞬变电磁法探测技术[J].煤炭科学技术,2015,43(1):104-107,73. YU Shi-jian.Transient electromagnetic method detecting technology of water-bearing occurence of aquifers in three-soft coal seam overlying rocks[J].Coal Science and Technology,2015,43(1):104-107,73.
[6]武 强,张志龙,马积福.煤层底板突水评价的新型实用方法—主控指标体系的建设[J].煤炭学报,2007,32(1):42-47. WU Qiang,ZHANG Zhi-long,MA Ji-fu.A new practical methodology of the coal floor water bursting evaluating Ⅱ-the master controlling index system constru-ction[J].Journal of China Coal Society,2007,32(1):42-47.
[7]武 强,殷作如.评价煤层顶板涌(突)水条件的“三图—双预测法”[J].煤炭学报,2000,25(1):60-65. WU Qiang,HUANG Xiao-ling,DONG Dong-lin.“Three maps-two predictions”method to evaluate water bursting conditions on roof coal[J].Journal of China Coal Society,2000,25(1):60-65.
[8]邱士利.基于GIS的岩溶地下水富水性评价方法研究[D].北京:中国地质科学院,2006. QIU Shi-li. Quantitative evaluation of karst groundwater yield property based on GIS technology[D].Beijing:Chinese Academy of Geological Sciences,2006.
[9]韩 超,泮晓华,李国梁.基于GIS多源信息集成的含水层富水性模糊层次分析法[J].水文地质工程地质,2012,39(4):19-25. HAN Chao,PAN Xiao-hua,LI Guo-liang,et al.The fuzzy analytic hierarchy process of water abundance of an aquifer based on GIS and multi-source information fusion techniques[J].Hydrogeology and Engineering Geology,2012,39(4):19-25.
[10]范立民,向茂西,彭 捷,等.西部生态脆弱矿区地下水对高强度采煤的响应[J].煤炭学报,2016,41(11):2672-2678. FAN Li-min,XIANG Mao-xi,PENG Jie,et al.Groundwater response to intensive mining in ecologically fragile area[J].Journal of China Coal Society,2016,41(11):2672-2678.
[11]彭 涛,宣良瑞,张海潮,等.卧龙湖煤矿砂岩含水层富水性预测及评价[J].煤矿安全,2014(8):199-202. PENG Tao,XUAN Liang-rui,ZHANG Hai-chao,et al.Prediction and evaluation of water abundance of sandstone aquifer in wolonghu coal mine[J].Coal & Safety,2012,39(4):19-25.
[12]范立民,王双明,刘社虎,等.榆神矿区矿井涌水量特征及影响因素[J].西安科技大学学报,2009,29(1):7-11. FAN Li-min,WANG Shuang-ming,LIU She-hu,et al.Outcome characteristics and influ-encing factor of coalmining wastewater in Yushen mining area[J].Journal of Xi'an University of Science and Technology,2009,29(1):7-11.
[13]邵亚红,姚多喜,鲁海峰,等.松散层底部含水层富水性评价[J].煤矿安全,2014,45(7):127-130. SHAO Ya-hong,YAO Duo-xi,LU Hai-feng,et al.Evaluation of water abundance of loose bed bottom aquifer[J].Safty in Coal Mines,2014,45(7):127-130.
[14]魏广庆.板集井田新生界底部松散层富水性分布规律及其对煤层开采影响研究[D].淮南:安徽理工大学,2005. WEI Guang-qing.Study on aquifer parameters of the lowermost Cenozoic unconsolidated strata in the Banji Coalfield and its influence on coal mining activites[D].Huainan:Anhui University of Science and Technology, 2005.
[15]刘瑞新.松散含水层下提高开采上限的研究与实践[J].煤炭科学技术,2010,38(11):56-59. LIU Rui-xin.Study and practices on improvement of mining up limit under loose aquifer[J].Coal Science and Technology,2010,38(11):56-59.
[16]李小龙,姚多喜.孙疃矿第四含水层分布特征及富水性评价[J].安徽理工大学学报(自然科学版),2013,33(4):15-19. LI Xiao-long,YAO Duo-xi.Distribution characteristics and evaluation of the fourth aquifer in Suntong[J].Journal of Anhui University of Science and Technology(Natural Science),2013,33(4):15-19.
[17]段 鹏.包气带岩性结构对地下水补给的影响研究[D].西安:长安大学,2013. DUAN Peng.The effect of soil texture and structure of vadose zone on recharge of groundwater[D].Xi'an:Chang'an University,2013.
[18]武 强,樊振丽.基于GIS的信息融合型含水层富水性评价方法——富水性指数法[J].煤炭学报,2011,36(7):1124-1128. WU Qiang,FAN Zhen-li.Water-richness evaluation method of water-filled aquifer based on the principle of information fusion with GIS:water-richness index method[J].Journal of China Coal Society,2011,36(7):1124-1128.
[19]李树忱,冯现大,李术才,等.矿井顶板突水模型试验多场信息的归一化处理方法[J].煤炭学报,2011,36(3):447-451. LI Shu-chen,FENG Xian-da,LI Shu-cai,et al.The normalization process of the multi-field information from a coal mine water-inrush model test[J].Journal of China Coal Society,2011,36(3):447-451.
[20]Steiner B L,Antolín F,Jacomet S.Testing of the consistency of the sieving(wash-over)process of waterlogged sediments by multiple operators[J].Journal of Archaeological Science Reports,2015,2:310-320.
[21]兰太权.再论“单位涌水量就是导水系数”[J].水文地质工程地质,2016,43(5):173-175 LAN Tai-quan.Revisit “the specific well yield is the transmissivity”[J].Hydro-Geology and Engineering Geology,2016,43(5):173-175.
[22]葛天民.关于导水系数讨论[J].勘察科学技术,1984(2):17. GE Tian-min.The discussion on specific capacity and the transmissivity[J].Exploration of Science and Technology,1984(2):17.
[23]Boucher M,Favreau G,Vouillamoz J M,et al.Estimating specific yield and transmissivity with magnetic resonance sounding in an unconfined sandstone aquifer(Niger)[J].Hydrogeology Journal,2009,17(7):1805-1815.
[24]朱芮芮,郑红星,刘昌明.黄土高原典型流域地下水补给-排泄关系及其变化[J].地理科学,2010,30(1):108-112. ZHU Rui-rui,ZHENG Hong-xing,LIU Chang-min.Changes of ground water recharge and discharge in watershed of the loess plateau[J].Scientia Geographica Sinica,2010,30(1):108-112.
[25]Chang C,Der Yeh H.Variability quantification of excess pressure head in heterogeneous deformable aquifers[J].Applied Mathematical Modelling,2016,40(19-20):8580-8591.
[26]Masetti M,Pedretti D,Sorichetta A,et al.Impact of a storm-water infiltration basin on the recharge dynamics in a highly permeable aquifer[J].Water Resources Management,2016,30(1):149-165.
[27]贺晓浪.小保当煤矿潜水含水层富水性及受采动影响分析[D].西安:西安科技大学,2016. HE Xiao-lang.Water-richness evaluation of unconfined aquifer and mining effects on the aquifer in Xiaobaodang coal mine[D].Xi'an:Xi'an University of Science and Technology,2016.
[28]吴永胜,哈 斯,乌格特茉勒.毛乌素沙地南缘沙丘表面径流特征[J].科学通报,2011,56(34):2917-2922. WU Yong-sheng, Hasi E, Wugetemole. Characteristics of surface runoff in a sandy area in southern Mu Us sandy land[J].Chinese Science Bulletin,2011,56(34):2917-2922.
[29]Nishigaki T,Sugihara S,Kilasara M,et al.Surface runoff generation and soil loss under different soil and rainfall properties in the Uluguru Mountains,Tanzania[J].Land Degradation and Development,2017,28(1):283-293.

相似文献/References:

[1]张典荣,李 静,张 佳,等.新型多用钻孔测斜仪的研制及应用[J].西安科技大学学报,2018,(02):224.[doi:10.13800/j.cnki.xakjdxxb.2018.0208]
 ZHANG Dian-rong,LI Jing,ZHANG Jia,et al.Development and application of new type multi-usage borehole inclinomlter[J].Journal of Xi'an University of Science and Technology,2018,(01):224.[doi:10.13800/j.cnki.xakjdxxb.2018.0208]
[2]赵 洲,魏江波.基于颗粒流方法的滑坡破坏机理与强度分析[J].西安科技大学学报,2018,(04):611.[doi:10.13800/j.cnki.xakjdxxb.2018.0414 ]
 ZHAO Zhou,WEI Jiang-bo.Landslide failure mechanism and intensityanalysis based on PFC2D[J].Journal of Xi'an University of Science and Technology,2018,(01):611.[doi:10.13800/j.cnki.xakjdxxb.2018.0414 ]
[3]刘之的,张伟杰,孙家兴,等.大情字井油田青一段特低渗透储层物性主控因素[J].西安科技大学学报,2018,(01):99.[doi:10.13800/j.cnki.xakjdxxb.2018.0115]
 LIU Zhi-di,ZHANG Wei-jie,SUN Jia-xing,et al.Factors influencing the physical properties of reservoir in the Qing 1 section of Daqingzijing Oilfield[J].Journal of Xi'an University of Science and Technology,2018,(01):99.[doi:10.13800/j.cnki.xakjdxxb.2018.0115]
[4]赵谦平,高 潮,尹锦涛,等.鄂尔多斯盆地下寺湾地区山西组泥页岩生气特征[J].西安科技大学学报,2018,(01):108.[doi:10.13800/j.cnki.xakjdxxb.2018.0116]
 ZHAO Qian-ping,GAO Chao,YIN Jin-tao,et al.Hydrocarbon generation characteristics of source rocksin Shanxi Formation of Xiasiwan Area,Ordos Basin[J].Journal of Xi'an University of Science and Technology,2018,(01):108.[doi:10.13800/j.cnki.xakjdxxb.2018.0116]
[5]赵乐义,杨 军,李 涛,等.酒泉盆地营尔凹陷下白垩统中沟组源储一体成藏条件[J].西安科技大学学报,2018,(01):118.[doi:10.13800/j.cnki.xakjdxxb.2018.0117]
 ZHAO Le-yi,YANG Jun,LI Tao,et al.Accumulation condition in source rock and reservoir of LowerCretaceousZhonggou Formation in Ying'er Sag of Jiuquan Basin[J].Journal of Xi'an University of Science and Technology,2018,(01):118.[doi:10.13800/j.cnki.xakjdxxb.2018.0117]
[6]曹 跃,刘延哲,段昕婷,等.定边地区延长组下部储层的沉积地质意义[J].西安科技大学学报,2018,(01):137.[doi:10.13800/j.cnki.xakjdxxb.2018.0119]
 CAO Yue,LIU Yan-zhe,DUAN Xin-ting,et al.Sedimentary geological significance of reservoir in the Lower Member of Yanchang Formation in Dingbian Area[J].Journal of Xi'an University of Science and Technology,2018,(01):137.[doi:10.13800/j.cnki.xakjdxxb.2018.0119]
[7]张 科,方 勇,陈全红,等.贝克盆地卫星重力场特征与构造单元划分[J].西安科技大学学报,2018,(01):145.[doi:10.13800/j.cnki.xakjdxxb.2018.0120]
 ZHANG Ke,FANG Yong,CHEN Quan-hong,et al.Satellite gravity field and the division of tectonic units of the Biak Basin,Indonesia[J].Journal of Xi'an University of Science and Technology,2018,(01):145.[doi:10.13800/j.cnki.xakjdxxb.2018.0120]
[8]于 波.鄂尔多斯盆地上古生界致密砂岩储层微观孔隙特征[J].西安科技大学学报,2018,(01):150.[doi:10.13800/j.cnki.xakjdxxb.2018.0121]
 YU Bo.Micro-characteristics of Upper Paleozoictight reservoir of Ordos Basin[J].Journal of Xi'an University of Science and Technology,2018,(01):150.[doi:10.13800/j.cnki.xakjdxxb.2018.0121]
[9]魏繁荣,张志东,吴向阳,等.陕北安塞地区延长组长8段裂缝发育特征[J].西安科技大学学报,2018,(06):975.[doi:10.13800/j.cnki.xakjdxxb.2018.0614]
 WEI Fan-rong,ZHANG Zhi-dong,WU Xiang-yang,et al.Development characteristics of fractures of Chang 8 member in Yanchang Formation in Ansai Area,North Shaanxi[J].Journal of Xi'an University of Science and Technology,2018,(01):975.[doi:10.13800/j.cnki.xakjdxxb.2018.0614]
[10]吴辰泓,张丽霞,高 潮.下寺湾地区延长组陆相页岩孔隙特征及影响因素[J].西安科技大学学报,2018,(06):990.[doi:10.13800/j.cnki.xakjdxxb.2018.0616]
 WU Chen-hong,ZHANG Li-xia,GAO Chao.Pore characteristics and influential factors on lacustrine shale in Yanchang Formation,Xiasiwan Area[J].Journal of Xi'an University of Science and Technology,2018,(01):990.[doi:10.13800/j.cnki.xakjdxxb.2018.0616]

备注/Memo

备注/Memo:
收稿日期:2018-03-20 责任编辑:李克永
基金项目:陕西省科技统筹创新工程计划项目(2014KTZB01-03-03)
通信作者:贺晓浪(1989-),男,陕西绥德人,博士研究生,E-mail:hexiaolang2010@163.com
更新日期/Last Update: 2019-02-28