利用地理空间数据分析预测地下水流动方向

Ana Daley, Arjun Ganesh, Juliet Holmes, Aparna Marathe
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引用次数: 0

摘要

地下水,即在地表下流动的水,提供了最大和最容易获取的淡水来源。当地下水受到污染时,污染物会分散,并与地下水的流动方向相同,直接威胁到饮用水和灌溉的完整性。所有地下水污染都会造成环境、健康和经济成本,但如果不及时减轻,这些成本可能会急剧增加。目前,确定污染物扩散方向的方法需要实地考察现场并测量地下水。本项目通过利用地理空间数据和统计学习方法来解决这一问题。这个项目的目的是双重的。首先,我们将美国各地与地下水流向相关的已知特征汇总到一个数据库中。拥有关于这些属性的集中数据源是对当前系统的改进,这些系统是稀疏的、不相交的,有时是不可访问的数据集。其次,我们将这些数据与机器学习技术相结合,开发了一个模型,该模型接受纬度和经度作为输入,并对美国境内任何地点的地下水流动方向进行预测。通过减少响应时间和总体缓解成本,准确的预测可以直接提高效率。我们利用两者之间最小的角度差异,根据已知的地下水流动方向验证了我们的模型预测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Predicting the Direction of Groundwater Flow Using Geospatial Data Analysis
Groundwater, water flowing beneath the Earth's surface, provides the largest and most accessed source of freshwater. When groundwater is contaminated, the pollutant will disperse and travel in the same direction as the flow of groundwater, which directly threatens the integrity of drinking water and irrigation. All instances of groundwater contamination incur environmental, health, and monetary costs, but when not mitigated promptly, these costs can increase drastically. Currently, the method for determining the direction a contaminant plume will travel requires physically visiting the site and surveying the groundwater. This project addresses this issue by leveraging geospatial data and statistical learning methods. The aims of this project were two-fold. First, we aggregated known features, relevant to the direction of groundwater flow, at sites across the United States into a database. Having a centralized source of data regarding these properties is an improvement on the current system of sparse, disjoint, and at times inaccessible data sets. Second, we utilized that data in conjunction with machine learning techniques to develop a model that receives latitude and longitude as inputs and generates a prediction of the direction of groundwater flow at any location within the United States. Having accurate predictions directly improves efficiency by reducing response times and overall mitigation costs. We validated our model predictions against the known direction of groundwater flow using the smallest angle differences between the two.
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