Affiliation:
1. Department of Earth System Science Stanford University Stanford CA USA
2. U.S. Geological Survey Denver CO USA
Abstract
AbstractMany individual measurement points are required to characterize groundwater velocity within an aquifer. Groundwater velocity is most commonly measured using a network of >5 cm diameter monitoring wells, which, if not already present at a site, are expensive and labor‐intensive to install. Drive‐point piezometers—simple, cost‐effective wells that can be installed by hand—are a common tool for sampling groundwater in shallow, alluvial aquifers, but most groundwater velocity measurement techniques require equipment that is too large for these narrow (usually <2 cm inside diameter) piezometers. In this technical note, we introduce a low‐cost sensor and well packer system (<$90 USD) for performing point dilution tests in narrow piezometers. Field data show that the magnitude of groundwater velocity measured with this technique agrees with velocities computed from natural gradient tracer tests. Additionally, with proper calibration, these sensors can be used to continuously monitor in‐well specific conductance, either during inter‐well tracer tests with saline tracers or for water quality monitoring. This system is a viable tool for rapid assessment of the magnitude of groundwater velocity in shallow aquifers.
Funder
National Science Foundation
Publisher
American Geophysical Union (AGU)
Subject
Water Science and Technology
Cited by
1 articles.
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