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<br /> <br />. <br /> <br />through the subsurface before entering stream <br />channels and flowing out of the watershed, <br />Integrating ground water into this "systems" <br />approach is essential, but challenging, because <br />of limitations in knowledge of the interactions <br />of ground water and surface water, These diffi- <br />culties are further complicated by the fact that <br />surface-water watersheds and ground-water <br />watersheds may not coincide, <br /> <br />To meet water-quality standards and criteria, <br />States and local agencies need to determine the <br />amount of contaminant movement (wasteload) <br />to surface waters so they can issue permits and <br />control discharges of waste, Typically, ground- <br />water inputs are not included in estimates of <br />wasteload; yet, in some cases, water-quality <br />standards and criteria cannot be met without <br />reducing contaminant loads from ground- <br />water discharges to streams, <br /> <br />. <br /> <br />It is generally assumed that ground water is <br />safe for consumption without treatment. <br />Concerns about the quality of ground water <br />from wells near streams, where contaminated <br />surface water might be part of the source of <br />water to the well, have led to increasing <br />interest in identifying when filtration or treat- <br />ment of ground water is needed, <br /> <br />Wetlands, marshes, and wooded areas along <br />streams (riparian zones) are protected in some <br />areas to help maintain wildlife habitat and <br />the quality of nearby surface water, Greater <br />knowledge of the water-quality functions <br />of riparian zones and of the pathways of <br />exchange between shallow ground water and <br />surface-water bodies is necessary to properly <br />evaluate the effects of riparian zones on water <br />quality. <br /> <br />. <br /> <br />CHARACTERISTICS OF <br />AQUATIC ENVIRONMENTS <br /> <br />. <br /> <br />Mixing of ground water with surface water can <br />have major effects on aquatic environments <br />if factors such as acidity, temperature, and <br /> <br />VII <br /> <br />dissolved oxygen are altered, Thus, changes in <br />the natural interaction of ground water and <br />surface water caused by human activities can <br />potentially have a significant effect on aquatic <br />environments. <br /> <br />. <br /> <br />The flow between surface water and ground <br />water creates a dynamic habitat for aquatic <br />fauna near the interface, These organisms <br />are part of a food chain that sustains a <br />diverse ecological community, Studies <br />indicate that these organisms may provide <br />important indications of water quality as <br />well as of adverse changes in aquatic <br />environments. <br /> <br />. <br /> <br />Many wetlands are dependent on a relatively <br />stable influx of ground water throughout <br />changing seasonal and annual weather <br />patterns. Wetlands can be highly sensitive to <br />the effects of ground-water development and <br />to land-use changes that modify the ground- <br />water flow regime of a wetland area, Under- <br />standing wetlands in the context of their asso- <br />ciated ground-water flow systems is essential <br />to assessing the cumulative effects of wetlands <br />on water quality, ground-water flow, and <br />streamflow in large areas. <br /> <br />The success of efforts to construct new <br />wetlands that replicate those that have been <br />destroyed depends on the extent to which the <br />replacement wetland is hydrologically similar <br />to the destroyed wetland, For example, the <br />replacement of a wetland that is dependent on <br />ground water for its water and chemical input <br />needs to be located in a similar ground-water <br />discharge area if the new wetland is to repli- <br />cate the original. Although a replacement <br />wetland may have a water depth similar to the <br />original, the communities that populate the <br />replacement wetland may be completely <br />different from communities that were present <br />in the original wetland because of differences <br />in hydrogeologic setting, <br /> <br />. <br />