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Journal of Groundwater Science and Engineering最新文献

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Mechanisms of Contaminant Transport in Aquifers 含水层中污染物运移机制
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2019-01-01 DOI: 10.1007/978-3-030-20516-4_10
R. Sethi, A. Molfetta
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引用次数: 1
Hydrochemical and isotope characteristics of spring water discharging from Qiushe Loess Section in Lingtai, northwestern China and their implication to groundwater recharge 灵台秋社黄土段泉水排泄的水化学和同位素特征及其对地下水补给的意义
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2017-12-01 DOI: 10.26599/jgse.2017.9280036
Chao Song, G. Han, Pan Wang, Yinggui Shi, Ze He
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引用次数: 1
A study on the supply relations of different groundwater in Qingdao subway line R3 青岛地铁R3线不同地下水供应关系研究
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2017-12-01 DOI: 10.26599/jgse.2017.9280037
Cao Lei, Zhaoqiang Gu, Shipeng Liu, Mingshuang Sun
In this paper, the correlation between different groundwater in the study area is analyzed by using the hydrological data from the hydrogeological test holes and the long-term observation holes based on the hydrogeological data between the Jinggangshan Road Station and the Jianianhua Station on the Qingdao Subway Line R3. The conclusions are as follows. When the drills are near the seashore (less than 50 m) and the backfilled formation has a large permeability coefficient (the backfilled components being coarse particles), the Quaternary pore water is connected with the seawater and there is correlation between the two. When the drills are far from the seashore (more than 50 m) or the backfilled formation has a small permeability coefficient, there is no correlation between the two. When the drills are near the seashore (less than 50 m) with developed bedrock fissure, the bedrock fissure water is connected with the seawater and there is correlation between the two. When the drills are far from the seashore (more than 50 m), or when the bedrock fissure is undeveloped, there is no correlation between the two. There exists an aquifer (mainly marine muddy silt clay layers and partially silt clay layers) between the Quaternary pore water and the bedrock fissure water, which blocks the connectivity between the two. Consequently, there is no correlation.
本文根据青岛地铁R3线井冈山路站至嘉年华站的水文地质资料,利用水文地质试验孔和长期观测孔的水文地质数据,分析了研究区不同地下水之间的相关性。结论如下。当钻机靠近海岸(小于50m),回填地层渗透系数大(回填成分为粗颗粒)时,第四系孔隙水与海水相通,二者存在相关性。当钻机远离海岸(超过50m)或回填地层的渗透系数较小时,两者之间没有相关性。当钻机靠近基岩裂隙发育的海岸(小于50m)时,基岩裂隙水与海水相通,两者之间存在相关性。当钻机远离海岸(超过50米)或基岩裂隙不发育时,两者之间没有相关性。第四系孔隙水与基岩裂隙水之间存在含水层(主要为海相淤泥质粉质粘土层,部分为粉质粘土),阻断了两者的连通性。因此,不存在相关性。
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引用次数: 0
Arsenic distribution and source in groundwater of Yangtze River Delta economic region, China 长三角地区地下水中砷的分布及来源
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2017-12-01 DOI: 10.26599/jgse.2017.9280034
Xu Zhou
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引用次数: 3
Clogging mechanism in the process of reinjection of used geothermal water: A simulation research on Xianyang No.2 reinjection well in a super-deep and porous geothermal reservoir 用过的地热水回注过程中的堵塞机理——以超深多孔地热储层咸阳2号回注井为例
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2017-12-01 DOI: 10.26599/jgse.2017.9280031
Zhiyuan Ma, Yong‐ping Xu, Mei-jing Zhai, M. Wu
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引用次数: 6
The Arc-view application in the field of hydrology and water resources 圆弧视图在水文水资源领域的应用
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2017-12-01 DOI: 10.26599/jgse.2017.9280038
Xiao-ming Wang, Fei Xue
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引用次数: 0
The comprehensive evaluation on resource environmental bearing capacity of central cities in the Yellow River Delta-A case study on Dongying City 黄河三角洲中心城市资源环境承载力综合评价——以东营市为例
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2017-12-01 DOI: 10.26599/jgse.2017.9280035
Kuifeng Wang, Meng Xu, Xiaoming Chen
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引用次数: 0
Analysis on variation characteristics of geothermal response in Liaoning Province 辽宁省地热响应变化特征分析
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2017-12-01 DOI: 10.26599/jgse.2017.9280033
Wei Zhu, W. Tang, Qiang Liu, Meiqiu Zhang
: Due to energy shortage and increasing environmental awareness, resources in shallow underground space have been rapidly exploited and utilized. So that studying variation characteristics of geothermal response in gneiss is necessary for effective and rational use of underground heat. Based on field test of thermal response in gneiss under hydrogeological survey project carried out in shallow geothermal energy development zone in Liaoning Province, this thesis analyzes mathematical statistics of geothermal response characteristics in main gneiss of Laoning Province. The initial formation temperature ranges from 10.80 ℃ to 15.80 ℃ according to field test. The statistical results show that in the condition of natural water content, the average thermal conductivity of Quaternary loose rocks comes as clay< silty< silty fine sand< medium sand< coarse sand< gravelly sand. This order is consistent with thermal conductivity characteristics of gneiss obtained in the laboratory. Formation temperature recovery in different strata follows as granite> medium sand> clay. This order is opposite to the absolute value of temperature recovery curve slope of corresponding lithology, which shows that the stratum with higher temperature recovery rate has lower temperature recovery curve slope.
:由于能源短缺和环保意识的提高,浅层地下空间的资源得到了迅速的开发和利用。因此,研究片麻岩地热响应的变化特征,对于有效、合理地利用地下热量是必要的。本文在辽宁省浅层地热能开发区水文地质调查项目的片麻岩热响应现场试验的基础上,对辽宁省主要片麻岩的热响应特征进行了数理统计分析。根据现场测试,初始地层温度在10.80℃至15.80℃之间。统计结果表明,在天然含水量条件下,第四系松散岩石的平均导热系数为粘土<粉土<粉细砂<中砂<粗砂<砾砂。该顺序与实验室获得的片麻岩的导热特性一致。不同地层的地层温度恢复规律为:花岗岩>中砂>粘土。该顺序与相应岩性的温度恢复曲线斜率的绝对值相反,表明温度恢复率越高的地层,温度恢复曲线的斜率越低。
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引用次数: 0
Research on the fault controlling mechanism of geothermal water in Zhangzhou Basin 漳州盆地地热水断裂控制机制研究
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2017-12-01 DOI: 10.26599/jgse.2017.9280032
H. Gan, Wenlin Lin, Gao Yue, Xiao Wang, Fengdi Ma, Gui-ling Wang
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引用次数: 2
Effect of climate change on the trends of evaporation of phreatic water from bare soil in Huaibei Plain, China 气候变化对淮北平原裸露土壤潜水蒸发趋势的影响
IF 1.1 4区 地球科学 Q3 WATER RESOURCES Pub Date : 2017-09-01 DOI: 10.26599/jgse.2017.9280021
Man-ting Shang, Peigui Liu, C. Lei, Ming-chao Liu, Liang Wu
{"title":"Effect of climate change on the trends of evaporation of phreatic water from bare soil in Huaibei Plain, China","authors":"Man-ting Shang, Peigui Liu, C. Lei, Ming-chao Liu, Liang Wu","doi":"10.26599/jgse.2017.9280021","DOIUrl":"https://doi.org/10.26599/jgse.2017.9280021","url":null,"abstract":"","PeriodicalId":43567,"journal":{"name":"Journal of Groundwater Science and Engineering","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2017-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46292570","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
期刊
Journal of Groundwater Science and Engineering
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