青海省格尔木山前平原区地下水动态特征分析

doi:10.7522/j.issn.1000-0240.2016.0027

冰川冻土 ›› 2016, Vol. 38 ›› Issue (1): 241-247.doi: 10.7522/j.issn.1000-0240.2016.0027

青海省格尔木山前平原区地下水动态特征分析

汪生斌^1,2, 肖勇³, 王万平^1,2, 祁泽学^1,2, 张婷婷^1,2, 赵文强^1,2

1. 青海省环境地质重点实验室, 青海西宁 810007;
2. 青海省环境地质勘查局, 青海西宁 810007;
3. 中国地质大学(北京) 水资源与环境学院, 北京 100083

收稿日期:2015-11-09 修回日期:2016-01-12 出版日期:2016-02-25 发布日期:2016-05-30
通讯作者: 肖勇,E-mail:cugbxy@163.com. E-mail:cugbxy@163.com
作者简介:汪生斌(1985-),男,青海湟中人,工程师,2013年在中国地质大学(北京)获工程硕士学位,主要从事水文地质、工程地质领域工作.E-mail:wangshengbin999@126.com
基金资助:
青海省重点城市(格尔木)环境地质调查评价(1212011140130)资助

Groundwater table dynamics in Golmud piedmont plain of Qinghai Province

WANG Shengbin^1,2, XIAO Yong³, WANG Wanping^1,2, QI Zexue^1,2, ZHANG Tingting^1,2, ZHAO Wenqiang^1,2

1. Key Lab of Geo-environment Qinghai Province, Xi'ning 810007, China;
2. Environmental Geological Prospecting Bureau of Qinghai Province, Xi'ning 810007, China;
3. School of Water Resources and Environment, China University of Geosciences, Beijing 10083, China

Received:2015-11-09 Revised:2016-01-12 Online:2016-02-25 Published:2016-05-30

摘要/Abstract

摘要： 在格尔木山前平原区水文地质条件基础上,结合多年地下水位监测资料,对格尔木河冲洪积平原区的多年水位动态特征及其影响因素进行了分析研究,总结出该地区的地下水动态类型.格尔木山前平原区3个不同区域由于赋存条件及开发利用条件的不同,地下水动态类型分异显著.研究区地下水整体流向与地形起伏相一致,自南向北径流,区域上流场形态变化不大.冲洪积扇中上部地下水多年动态处于平衡状态,近年来由于开采力度加大,地下水位呈急速下降趋势,地下水动态类型为水文-径流型;冲洪积扇下部地下水位以区域性下降为主,地下水动态类型主要为蒸发型;冲洪积扇西翼水源地附近由于地下水调蓄能力较强,地下水位总体呈稳定并局部有上升趋势,地下水动态类型为水文-人类活动型.

关键词: 地下水位, 动态成因类型, 山前平原区, 格尔木

Abstract: Based on the study of hydrogeological condition in Golmud piedmont pain, the annual groundwater level and its control factors were analyzed. The temporal-spatial variations of groundwater level from 1990 to 2013 were analyzed and the groundwater dynamic types were summarized. Due to the different storage conditions and exploitation degrees, the groundwater types are remarkably different in the three study subregions. The groundwater flow direction is from south to north, which is consistent with the terrain, and the regional flow field has varied less during the last five years. The annual groundwater variation in the upper and middle regions of the alluvial-proluvial fan remains in equilibrium state, while the groundwater level has decreased sharply due to the over-exploitation in the last few years, and the groundwater dynamic type is hydrological-runoff type. The groundwater level in the lower part of the alluvial-proluvial fan has decreased and the groundwater dynamic type is evaporation type mainly. The groundwater level in the western part of the alluvial-proluvial fan has remained stable and increased in some parts due to the strong regulation and storage capacity of the aquifer, the groundwater dynamic type is hydrological-exploitation type.

Key words: groundwater level, dynamic genetic types, piedmont plain, Golmud

中图分类号:

P641.74

汪生斌, 肖勇, 王万平, 祁泽学, 张婷婷, 赵文强. 青海省格尔木山前平原区地下水动态特征分析[J]. 冰川冻土, 2016, 38(1): 241-247.

WANG Shengbin, XIAO Yong, WANG Wanping, QI Zexue, ZHANG Tingting, ZHAO Wenqiang. Groundwater table dynamics in Golmud piedmont plain of Qinghai Province[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2016, 38(1): 241-247.

参考文献

[1] Li Jisheng, Hu Xinglin, Huang Weidong, et al. Variation and trend prediction of the mountain runoffs of the trunk streams of the Shule River basin, Hexi Corredor[J]. Journal of Glaciology and Geocryology, 2015, 37(3): 803-810.[李计生, 胡兴林, 黄维东,等. 河西走廊疏勒河流域出山径流变化规律及趋势预测[J]. 冰川冻土, 2015, 37(3): 803-810.]
[2] Abulimiti Ablikim, Zhou Jingwu. Surface discharge characteristics of the Turpan Basin, Xinjing[J]. Journal of Glaciology and Geocryology, 2014, 36(3): 717-723.[阿不力米提·阿不力克木, 周京武. 新疆吐鲁番盆地地表径流特征[J]. 冰川冻土, 2014, 36(3): 717-723.]
[3] Apaydin H, Sonmez F K, Yildirim Y E. Spatial interpolation techniques for climate data in the GAP region in Turkey[J]. Climate Research, 2004, 28(1): 31-40.
[4] Mi Lina, Xiao Honglang, Zhu Wenjing, et al. Dynamic variation of the groundwater level in the middle reaches of the Heihe River during 1985-2013[J]. Journal of Glaciology and Geocryology, 2015, 37(2): 461-469.[米丽娜, 肖洪浪, 朱文婧, 等. 1985-2013年黑河中游流域地下水位动态变化特征[J]. 冰川冻土, 2015, 37(2):461-469.]
[5] Gates J B, Edmunds W M, Darling W G, et al. Conceptual model of recharge to southeastern Basin Jaran Desert groundwater and lakes from environmental tracers[J]. Applied Geochemistry, 2008, 23(12) : 3519-3534.
[6] Ma Jinzhu, Ding Zhenyu, Edmunds W M, et al. Limits to recharge of groundwater from Tibetan plateau to the Gobi desert, implications for water management in the mountain front[J]. Journal of Hydrology, 2009, 364(1): 128-141.
[7] Scanlon B R, Keese K E, Flint A L, et al. Global synthesis of groundwater recharge in semiarid and arid regions[J]. Hydrological processes, 2006, 20(15): 3335-3370.
[8] Wang Yuhang, Wang Wenke, Duan Lei, et al. Study on dynamic of groundwater in alluvial-pluvial fan zone in front of mountain of Golmud River basin[J]. Journal of Water Resources & Water Engineering, 2014, 25(1): 133-136.[王宇航, 王文科, 段磊, 等. 格尔木河流域山前冲洪积扇地下水动态研究[J]. 水资源与水工程学报, 2014, 25(1): 133-136.]
[9] Song Ru. The application of kriging method to studying dynamic observation network of groundwater level regime in Geermu River region[J]. Coal Geology of China, 1997, 9(4): 39-42.[宋儒. 应用Kriging方法研究格尔木河流域地下水位动态观测网的优化配置[J]. 中国煤炭地质, 1997, 9(4): 39-42.]
[10] Xue Jianjun. Grey relational analysis of groundwater level in Golmud area[J]. Journal of Hydrology and Water Resources, 2001, 22(3): 4-5.[薛建军. 格尔木地区地下水水位的灰关联分析[J]. 水文水资源, 2001, 22(3): 4-5.]
[11] Luo Yinfei. The groundwater system and resources in piedmont plain of Golmud River Basin in Qinghai Province[D]. Beijing: China University of Geosciences (Beijing), 2013.[罗银飞. 青海省格尔木河流域山前平原区地下水系统及地下水资源评价[D].北京: 中国地质大学(北京), 2013.]
[12] Wang Shengbin. The reason of groundwater level rising and prevention measure in Golmud[J]. West-China Exploration, 2012, 24(8): 179-180.[汪生斌. 格尔木市地下水位上升的初步原因及防治对策[J]. 西部探矿工程, 2012, 24(8): 179-180.]
[13] Wang Yuhang. Geochemistry evolution and water cycle patterns of groundwater in Golmud River basin[D]. Xi'an: Chang'an University, 2014.[王宇航. 格尔木河流域地下水化学演化规律和水循环模式[D]. 西安: 长安大学, 2014.]
[14] Deng Mingjiang, Pei Jiansheng, Wang Zhi, et al. Under groundwater regulation and storage system and water resources exploitation-utilization mode of continental river basins in arid areas[J]. Arid Land Geography, 2007, 30(5): 621-628.[邓铭江, 裴建生, 王智, 等. 干旱区内陆河流域地下水调蓄系统与水资源开发利用模式[J]. 干旱区地理, 2007, 30(5): 621-628.]
[15] Huang Jinting. The responses of evapotranspiration to the groundwater changes in the semi-arid area[D]. Xi'an: Chang'an University, 2013.[黄金廷. 半干旱区蒸散发对地下水变化响应机制研究[D]. 西安: 长安大学, 2013.]
[16] Huo Aidi, Hou Ming, Deng Hongzhang. Research on evapotranspiration and groundwater level variation of Golmud[C]. Water Resources Management and Engineering International Conference Proceedings, 2011.[霍艾迪, 侯明, 邓宏章. 格尔木地区地表蒸散量与地下水位变化关系研究[C]. 水资源管理与工程国际学术会议论文集, 2011.]
[17] Liu Guangming, Yang Jingsong, Li Dongshun. Evaporation regularity and its relationship with soil salt[J]. Acta Pedologica Sinica, 2002, 39(3): 384-389.[刘广明, 杨劲松, 李冬顺. 地下水蒸发规律及其与土壤盐分的关系[J]. 土壤学报, 2002, 39(3): 384-389.]
[18] Ma Jinzhu, Li Jijun, Gao Qianzhao. Groundwater evolution and its influence on eco-environment under climatic change and human activity in the south of Tarim Basin[J]. Arid Land Geography, 2004, 25(1): 16-23.[马金珠, 李吉均, 高前兆, 等. 气候变化与人类活动干扰下塔里木盆地南缘地下水的变化及其生态环境效应[J]. 干旱区地理, 2004, 25(1): 16-23.]
[19] Ma Jinzhu, Li Jijun. Impact of human activities on groundwater and the effect on eco-environment in southern Tarim Basin[J]. Journal of Natural Resources, 2001, 16(2): 134-139.[马金珠, 李吉均. 塔里木盆地南缘人类活动干扰下地下水的变化及其生态环境效应[J]. 自然资源学报, 2001, 16(2): 134-139.]
[20] Wang Wenke, Luan Yuesheng, Yang Zeyuan, et al. Influence on water resource and eco-environment system of Geermu alluvial fan by great artificial projects[J]. Journal of Xi'an Engineering University, 2001, 23(2): 6-11.[王文科, 栾约生, 杨泽元, 等. 人类重大工程对格尔木冲洪积扇水资源与生态环境系统的影响研究[J]. 西安工程学院学报, 2001, 23(2): 6-11.]

青海省格尔木山前平原区地下水动态特征分析

Groundwater table dynamics in Golmud piedmont plain of Qinghai Province

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 6

Metrics

本文评价

推荐阅读 0

[1]	米丽娜, 肖洪浪, 朱文婧, 李计生, 肖生春, 李丽莉. 1985-2013年黑河中游流域地下水位动态变化特征[J]. 冰川冻土, 2015, 37(2): 461-469.
[2]	姚兴荣, 丁宏伟, 沈永平, 蓝永超, 赵玉苹, 曹晓辉, 尹政. 黑河干流拟建水利工程对下游生态环境的影响分析[J]. 冰川冻土, 2012, 34(4): 934-941.
[3]	吉喜斌, 康尔泗, 陈仁升, 赵文智, 金博文, 张智慧. 黑河中游灌区地下水位短期季节性变化趋势预测[J]. 冰川冻土, 2006, 28(3): 421-427.
[4]	庄丽, 陈亚宁, 李卫红, 袁素芬. 干旱区荒漠植被丙二醛及保护酶活性对地下水位的响应[J]. 冰川冻土, 2005, 27(5): 723-733.
[5]	张宏锋, 陈亚宁, 李卫红, 陈亚鹏. 塔里木河下游物种多样性与地下水位灰色关联分析[J]. 冰川冻土, 2004, 26(6): 705-712.
[6]	彭轩明, 吴青柏, 田明中. 黄河源区地下水位下降对生态环境的影响[J]. 冰川冻土, 2003, 25(6): 667-671.