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ABSTRACT: Boris Faybishenko of Berkeley Lab has developed an omni-depth fluxmeter to provide direct field measurements of water and concentration flux at different depths in the vadose zone. Conventional methods to obtain this information require taking samples for laboratory analysis or calculations, which may lead to large inaccuracies. Other in situ fluxmeters are limited to measurements in near-saturated soils or require a preliminary calibration of probes. The Berkeley Lab vadose zone fluxmeter measurements are based on establishing the same water pressure on a tensiometer placed inside a controlled soil environment as that exerted naturally on a monitoring tensiometer located in undisturbed soil. This fluxmeter can fit into a borehole four inches in diameter or larger and is accurate to within 10 percent, if water pressure is above approximately - 0.7 bars. An innovative arrangement for large boreholes consists of
two semi-sheltered fluxmeters, one facing upward and one downward,
monitoring tensiometers placed in undisturbed soil, and a
vacuum-operated data acquisition system. The Berkeley Lab fluxmeter enables farmers to monitor water flux and chemical concentrations in soil, which in turn allows them to optimize irrigation and drainage schedules, as well as adjust pesticide and fertilizer applications to minimize groundwater contamination. The fluxmeter can also be used in monitoring and managing remediation of contaminated soils, and mine tailing and landfill operations.
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FOR MORE INFORMATION PLEASE SEE:
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REFERENCE NUMBER: IB-1599 |
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