The second susceptibility occurs under distributing pumping conditions, during which significant reductions in groundwater elevations are apparent in narrow valleys (Fig. 8D). Again, this is most likely associated with the aquifer geometry and area of contributing recharge. As demonstrated in Fig. 7, increases in both development density and water volume per pad elicit heightened water table responses; this trend was shared by all sources. Although water table change was still undetectable for stream withdrawals at the maximum development tested,

heightened resolution and smaller scale models might allow for Staurosporine better understanding of the connection between streams and groundwater. Changes to stream flow in response to high-volume water withdrawals are spatially selleck products variable. The most significant reduction to stream flow is concentrated in one region of the model (Fig. 9, cross-sections 7, 8, and 9). Other areas of the model respond relatively uniformly to extraction scenarios, with the percent reduction in stream flow increasing with increasing development density and water volume per pad. Within the minimum development range, extracting water from both municipal pumping wells and streams

reduces stream flow by less than 2% throughout most of the stream network (Fig. 9A). At the maximum density of development, stream flow is reduced by up to 13% in a localized region (Fig. 9D). Under those same development conditions, however, stream flow reduction still remains under 3% throughout most of the stream network. Although the magnitude of stream flow reduction changes N-acetylglucosamine-1-phosphate transferase based on water source, the general spatial distribution persists (Fig. 10). Streams throughout the model respond consistently to applied withdrawal scenarios with the exception of stream cross-sections 7, 8, and 9, which exhibit nearly three times the stream flow reduction as compared to the rest of the stream segments. The combination source and stream withdrawals produced the greatest response in stream flow whereas distributed

pumping scenario results in a less dramatic response (Fig. 10). Extracting from municipal wells causes more spatial variability in stream flow reduction as compared to the combination source (Fig. 10, cross-section 8). There is a positive relationship between stream flow reduction and volume of extracted water which is determined by both well pad density and water volume per pad. Relatively uniform response throughout most of the stream segments emphasizes the markedly greater response at cross-sections 7, 8, and 9 (Fig. 9). These locations are in narrow valleys and represent streams with lesser annual discharge. These two factors dictate the capacity of groundwater–surface water exchange when withdrawals from either the aquifer or the streams are applied. Downstream parts of the stream network (Fig.