首页> 外文会议>Symposium on the Application of Geophysics to Engineering and Environmental Problems >COMBINED USE OF FREQUENCY-DOMAIN ELECTROMAGNETIC ANDELECTRICAL RESISTIVITY SURVEYS TO DELINEATE THEFRESHWATER/SALTWATER INTERFACE NEAR SALINE LAKES IN THENEBRASKA SAND HILLS, NEBRASKA, USA
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COMBINED USE OF FREQUENCY-DOMAIN ELECTROMAGNETIC ANDELECTRICAL RESISTIVITY SURVEYS TO DELINEATE THEFRESHWATER/SALTWATER INTERFACE NEAR SALINE LAKES IN THENEBRASKA SAND HILLS, NEBRASKA, USA

机译:频率域电磁电阻电阻率调查的结合使用绘制The Brasha Sand Hills的盐水湖附近的商品/盐水界面

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We investigate the use of frequency-domain electromagnetic (FDEM) and electrical resistivity (ER) surveys for rapid and detailed characterization of the direction of lake-aquifer fluxes and the configuration of salt plumes generated from saline lakes. This methodology was developed and applied at several lakes in the Nebraska Sand Hills, Nebraska, in an area with both freshwater and saline lakes hydraulically connected to the freshwater surficial aquifer. The FDEM survey was conducted by mounting the instrument on a fiberglass cart towed by an all-terrain vehicle. The towed FDEM surveys covered about 25 km per day and served as a reconnaissance method for choosing locations for the more quantitative and detailed ER surveys. Around the saline lakes, areas with high electrical conductivity are consistent with the regional direction of ground-water flow. Lower electrical conductivity was measured around the freshwater lakes with anomalies correlating to a paleovalley axis inferred from previous studies. The efficacy of this geophysical approach is attributed to: (1) significant contrast in electrical conductivity between freshwater and saltwater, (2) near-surface location of the freshwater/saltwater interface, (3) minimal cultural interference, and (4) relative homogeneity of the aquifer materials.
机译:我们调查使用频域电磁(FDEM)和电阻率(ER)调查的使用,以便快速,详细地表征湖泊含水液相传,以及盐水湖中产生的盐羽毛的配置。这种方法是在内布拉斯加州内布拉斯加州的几个湖泊中开发和应用,在一个淡水和盐水湖泊的一个地区,液压连接到淡水表达含水层。通过将仪器安装在由全地形车辆牵引的玻璃纤维推车上进行FDEM调查。拖曳的FDEM调查每天覆盖约25公里,并作为选择更多定量和详细的ER调查的地点的侦察方法。在盐水湖周围,电导率高的区域与地下水流动的区域方向一致。在淡水湖周围测量较低的导电率,异常与从以前的研究推断出古价统一轴的异常。这种地球物理方法的疗效归因于:(1)淡水和盐水之间的导电性显着对比,(2)淡水/盐水界面的近表面位置,(3)最小的文化干扰,(4)相对均匀性含水层材料。

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