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Estimation of water table depth using DUALEM-2 system

机译:使用Dualem-2系统估算水位深度

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Most of the agricultural fields are generally irrigated or drained uniformly without considering the spatial and temporal variation in water table depth (WTD). Investigating WTD is important for scheduling irrigation, drainage system designs and water balance models. The objective of this study was to develop a software interface to estimate the variations in WTD via electromagnetic induction (EMI) methods using frequencies of a DUALEM-2 system. Two fields (Field 1: 45.38 degrees N, 63.23 degrees W and Field 2: 45.37 degrees N, 63.25 degrees W) were selected and thirty perforated observation wells were installed to calibrate the DUALEM-2 for predicting WTD. Boundaries of the selected sites and location of the wells were marked using a real time kinematics global positioning system (RTK-GPS). The user interface program was developed in Delphi 5.0 software and imported in a laptop computer to retrieve data from the DUALEM-2 system. The horizontal co-planar (HCP) geometry, perpendicular co-planar (PRP) geometry and WTD were recorded simultaneously from each well before and after every significant rainfall for three consecutive days. Comprehensive surveys were conducted to measure apparent ground conductivity (ECa) with DUALEM-2 and corresponding locations of the sampling points using Trimble Ag GPS 332. The regression model showed significant correlation between the HCP and WTD with co-efficient of determination (R-2 = 0.71) for field 1 and (R-2 = 0.53) for field 2. Maps were generated in ArcGIS 10 software to examine the accuracy of predicted WTD in comparison with actual values. Results indicated that the DUALEM-2 system was efficient in mapping variation rapidly and reliably in WTD in a non-destructive fashion rather than following conventional way of repeated well drilling for WTD determination. This information could be used for measuring the depletion of WTD during dry periods (droughts), site-specific irrigation and drainage design with the aided advantage of labor and time savings in case of observing precision water management practices at large fields.
机译:大多数农业领域通常灌溉或均匀地排出,而不考虑水位深度(WTD)的空间和时间变化。调查WTD对于调度灌溉,排水系统设计和水平衡模型非常重要。本研究的目的是开发一种软​​件界面,以估计通过Dualem-2系统的频率通过电磁感应(EMI)方法的WTD变化。选择两个场(字段1:45.38,63.23度和字段2:45.37度N,63.25°W),并安装了30个穿孔观察孔以校准Dualem-2以预测WTD。使用实时运动学全球定位系统(RTK-GPS)标记所选网站的边界和孔的位置。用户界面程序是在Delphi 5.0软件中开发的,并在笔记本电脑中导入,从Dualem-2系统中检索数据。水平共平面(HCP)几何形状,垂直的共平面(PRP)几何和WTD在连续三天之前和之后同时从每个孔中记录。进行综合调查以测量具有Dualem-2的表观接地电导率(ECA),并使用Trimble Ag GPS 332测量采样点的相应位置。回归模型显示HCP和WTD之间的显着相关性,确定测定的共同效率(R-2用于字段1的字段1和(R-2 = 0.53)的= 0.71)。在ArcGIS 10软件中生成映射,以检查预测WTD的准确性与实际值相比。结果表明,Dualem-2系统以非破坏性方式在WTD中迅速可靠地绘制变化而不是常规方法,而不是在重复钻井中进行WTD测定。该信息可用于测量干燥时期(干旱),现场特定灌溉和排水设计期间WTD的耗竭,以便在大田观察精密水管理实践的情况下劳动和时间节省的辅助优势。

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