Item talk:Q257556
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"name": "Groundwater and surface-water interactions in the He\u2018eia watershed, O\u2018ahu, Hawai\u2018i\u2014Insights from analysis of historical data and numerical groundwater-model simulations",
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"abstract": "He\u2018eia and \u2018Ioleka\u2018a Streams in the He\u2018eia watershed on O\u2018ahu, Hawai\u2018i, receive substantial discharge from dike-impounded groundwater. Previous studies indicated that groundwater withdrawals from the watershed affect streamflow. Resource managers and users seek information that can be used to balance the needs of competing uses of groundwater and streamflow in the watershed.In this study, analyses of historical streamflow and withdrawal data indicate that when groundwater withdrawals from Haiku Tunnel (a groundwater development tunnel built in the 1940s in the watershed) of 1.73\u20131.87 million gallons per day (Mgal/d) were introduced in the first few decades of the tunnel\u2019s operation, base flow at a gage on He\u2018eia Stream decreased by 1.37\u20131.40 Mgal/d. Changes in rainfall during this period were not sufficient to account for the changes in base flow. The tunnel withdrawal also affected \u2018Ioleka\u2018a Stream, but the effect was less. In the 1980s, average withdrawal from the tunnel decreased by 0.73\u20131.00 Mgal/d and base flow at the He\u2018eia streamgage increased by 0.15\u20130.21 Mgal/d; a concurrent rainfall increase may partly account for the base-flow increase. Withdrawal from another well (Haiku well) starting in the late 1980s had a much smaller effect than the tunnel did on flow at the He\u2018eia streamgage.Numerical groundwater-model simulations indicate that shutting down withdrawals from Haiku Tunnel and Haiku well would increase base flows in streams inside and outside of the He\u2018eia watershed. Simulated shutdown of 0.35 Mgal/d withdrawal from Haiku well caused base flow of streams in the He\u2018eia watershed to increase by 0.09 Mgal/d or 26 percent of the withdrawal reduction, and shutdown of 0.60 Mgal/d withdrawal from Haiku Tunnel caused base flow of streams within the watershed to increase by 0.12 Mgal/d or 20 percent of withdrawal reduction. Shutdown of a combined 0.95 Mgal/d withdrawal from the tunnel and well caused base flow of streams within the watershed to increase by 0.22 Mgal/d or 23 percent of the withdrawal reduction.The model simulations and analyses of streamflow data demonstrate that, climate changes notwithstanding, reducing or shutting down withdrawal from Haiku Tunnel has not in the past, and will not in the future, restore base flow to predevelopment rates. The nearly pristine condition that existed prior to the construction of the Haiku Tunnel no longer exists because other large-producing tunnels and wells near the He\u2018eia watershed have since begun withdrawing water from the same dike-impounded aquifer. Reduction or shutdown of withdrawals from the wells and tunnel in the He\u2018eia watershed cannot restore streamflow to predevelopment rates if withdrawals from all other wells and tunnels continue.",
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