Arid
DOI10.1007/s10064-020-01805-y
Laboratory characterization of sandy soil water content during drying process using electrical resistivity/resistance method (ERM)
An, Ni1,2; Tang, Chao-Sheng1; Cheng, Qing1; Wang, De-Yin1; Shi, Bin1
通讯作者Tang, Chao-Sheng
来源期刊BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT
ISSN1435-9529
EISSN1435-9537
出版年2020
卷号79期号:8页码:4411-4427
英文摘要Drought-induced evaporation can reduce soil water content and significantly alter soil hydro-mechanical behavior. Understanding the temporal and spatial distribution characteristics of soil water content during evaporation is of great significance for evaluating the encountered geotechnical and geo-environmental problems in arid or semi-arid regions. In this study, an electrical resistivity/resistance method (ERM) with a high spatial resolution of centimeter-level was developed for a small-scale laboratory test and applied to quantitatively characterize the evaporation-induced water content variations along a depth gradient. A total of 8 groups of initially saturated sandy soil columns (84 mm in diameter and 290 mm in height) were prepared, and eight pairs of mini electrodes (3.5 mm in diameter) were installed in each soil sample with a vertical distance of 30 mm. The soil columns were subjected to continuous drying. The changes in soil electrical resistance at different depths were monitored by the electrode couples. The gravimetric water contents at different depths were also measured at the end of drying. It is found that soil water content decreases exponentially with increasing electrical resistance. Based on the obtained data, a calibration relationship between soil gravimetric water content and corrected electrical resistance was well established with consideration of temperature effect. This relationship was validated successfully by the experimental results, indicating the feasibility of the developed ERM to characterize the soil water content dynamics during the drying process. Besides, the drying process with the movement of the evaporation front was discussed. The results of this study demonstrate the good performance of ERM in the estimation of temporal and spatial variations of soil water content and its potential application in arid or semi-arid regions with frequent droughts.
英文关键词Soil water evaporation Soil water content Electrical resistivity resistance method (ERM) Evaporation front Temperature effect
类型Article
语种英语
国家Peoples R China ; Wales
收录类别SCI-E
WOS记录号WOS:000531230300002
WOS关键词BARE-SOIL ; DC RESISTIVITY ; CLAYEY SOIL ; TEMPERATURE-CHANGES ; EVAPORATIVE FLUXES ; SURFACE-RESISTANCE ; NUMERICAL-ANALYSIS ; SOLUTE TRANSPORT ; TOMOGRAPHY ERT ; CONDUCTIVITY
WOS类目Engineering, Environmental ; Engineering, Geological ; Geosciences, Multidisciplinary
WOS研究方向Engineering ; Geology
来源机构南京大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/319076
作者单位1.Nanjing Univ, Sch Earth Sci & Engn, 163 Xianlin Ave, Nanjing 210023, Peoples R China;
2.Cardiff Univ, Geoenvironm Res Ctr, Cardiff Sch Engn, Newport Rd, Cardiff CF24 3AA, Wales
推荐引用方式
GB/T 7714
An, Ni,Tang, Chao-Sheng,Cheng, Qing,et al. Laboratory characterization of sandy soil water content during drying process using electrical resistivity/resistance method (ERM)[J]. 南京大学,2020,79(8):4411-4427.
APA An, Ni,Tang, Chao-Sheng,Cheng, Qing,Wang, De-Yin,&Shi, Bin.(2020).Laboratory characterization of sandy soil water content during drying process using electrical resistivity/resistance method (ERM).BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT,79(8),4411-4427.
MLA An, Ni,et al."Laboratory characterization of sandy soil water content during drying process using electrical resistivity/resistance method (ERM)".BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT 79.8(2020):4411-4427.
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[An, Ni]的文章
[Tang, Chao-Sheng]的文章
[Cheng, Qing]的文章
百度学术
百度学术中相似的文章
[An, Ni]的文章
[Tang, Chao-Sheng]的文章
[Cheng, Qing]的文章
必应学术
必应学术中相似的文章
[An, Ni]的文章
[Tang, Chao-Sheng]的文章
[Cheng, Qing]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。