THE EFFECT OF TRANSIENT RECHARGE ON SIMULATED ADVECTIVE TRANSPORT OF EXPLOSIVE COMPOUNDS IN GROUND WATER AT CAMP EDWARDS, CAPE COD, MASSACHUSETTS
Time-varying recharge can change heads in the aquifer and shift the position of the top of the water-table mound. As a result, hydraulic gradients and ground-water-flow lines in the aquifer can change through time. Transient modeling at the site has shown that ground-water-flow patterns in areas downgradient of the water-table mound and closer to discharge boundaries, where hydraulic gradients are steeper, are not greatly affected by changes in recharge. Ground-water-flow patterns in areas near the top of the water-table mound, where gradients are small, can change with time; particles released from the same location at different times can take different paths. Comparisons of steady-state and transient particle tracks indicate that calibrated steady-state models are sufficient to simulate advective transport in downgradient areas of the site, whereas steady-state models may not accurately simulate advective transport near the top of the water-table mound.