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Published byAngela Pierce Modified over 8 years ago
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Today’s Lecture Water levels and groundwater flow
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Announcements Lecture today: groundwater flow Thursday: guest lecture Joy Jenkins, EPA: Captain Jack Superfund site Lab Lab 1: Phase I ESA rewriting? Lab 2: Surface water sampling grading in progress? Lab 3: Soil sampling report due Wed Oct 21 Lab 4: Well drilling report due Fri Oct 30
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Announcements Lab Wednesday, Oct 28 Lab 5 Groundwater sampling / Slug test East campus
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Water Levels and Groundwater Flow Measuring water levels in wells single measurements electronic water level sensors simple tape measures inaccurate long-term monitoring pressure transducers data recorders
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Water Levels and Groundwater Flow Water level meters sensors on tapes weighted probe on marked tape (PVDF*) water completes circuit across electrodes buzzer, light notification depth relative to known elevation; e.g., top of well casing depths to 1,000 ft accuracy to 0.01 ft or 1 mm * polyvinylidene difluoride
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Water Levels and Groundwater Flow Water level meters advantages reliable, rugged easy to operate accurate disadvantages probe, tape catches on casing joints false readings from cascading water, condensation a lot of reeling!
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Water Levels and Groundwater Flow Water level meters sounders (acoustic) travel time for sound wave low frequency (50-200 Hz) depth relative to known elevation; e.g., top of well casing accuracy to 0.01 ft or 1 mm advantages quick; no decontamination disadvantages reflections off untrue well casing
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Water Levels and Groundwater Flow Long-term monitors pressure transducers accuracy 0.05% temperature compensation barometric compensation data loggers 100,000s of readings
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Water Levels and Groundwater Flow
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Groundwater flow contours contours of groundwater elevation potentiometric surface of surficial aquifer less relevant for confined aquifers direction and velocity of groundwater flow important for contaminant transport less useful for DNAPLs
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Water Levels and Groundwater Flow Groundwater flow contours water flows from high to low head often follows topography, but not always slope hydraulic gradient (L/L) direction planar surface defined by at least three water level measurements
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 28.1 ft 28.8 ft 28.4 ft
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 28.1 ft 28.8 ft 28.4 ft 170 ft
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 27.9 ft 28.8 ft 28.2 ft 170 ft
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 27.9 ft 28.8 ft 28.2 ft 170 ft 113 ft
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 27.9 ft 28.8 ft 28.2 ft 170 ft 113 ft
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 27.9 ft 28.8 ft 28.2 ft 170 ft 113 ft
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 27.9 ft 28.8 ft 28.2 ft 170 ft
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 27.9 ft 28.8 ft 28.2 ft 170 ft 28.7 ft 76 ft
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 27.9 ft 28.8 ft 28.2 ft 170 ft 28.7 ft 76 ft
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Water Levels and Groundwater Flow Calculation of groundwater flow direction water levels in three wells 27.9 ft 28.8 ft 28.2 ft 170 ft 28.7 ft 76 ft
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Water Levels and Groundwater Flow Groundwater Flow Calculator doi: 10.1111/gwat.12211
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Water Levels and Groundwater Flow Groundwater Flow Calculator
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Water Levels and Groundwater Flow Groundwater Flow Calculator
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Water Levels and Groundwater Flow Errors in groundwater level measurement recording and transcription errors condensation in well casing poor flow through well screen nearby infiltration sources water line leaks presence of LNAPL (“free product”) leads to errors in groundwater velocity and direction LNAPL
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Next Lecture Guest lecture Measuring aquifer properties – slug tests
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