沿着加利纳斯河地表水和地下水路径的水质评估,拉斯维加斯,新墨西哥

T. Evans, Daryl Williams, J. Lindline
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引用次数: 1

摘要

我们报告了一项试点研究的初步结果,该研究比较了加利纳斯流域地表水和地下水的化学成分。加利纳斯河发源于桑格雷德克里斯托山脉南部,向东南流向新墨西哥州拉斯维加斯的高平原沙漠社区。很大一部分水被分流到斯托里湖水项目,并分配给多个用户,包括拉斯维加斯市、拉斯维加斯国家野生动物保护区、农民和牧场主。我们研究了引水系统不同区域内的水质变化。在四个主要地点采集样本:地表水源(上加利纳斯河)、改道地表水(McCallister湖)、地下水渗漏(沿加利纳斯峡谷的泉水)和地下水受体(下加利纳斯河)。该研究假设,随着水渗透到地下,该地区的高碱性土壤和浅层基岩含水层为地下水提供了溶解成分。为了验证这一假设,我们收集了加利纳斯河水源的地表水和地下水样本,并对各种水参数进行了分析。结果表明,地下水中Ca、Mg、Na、Si、Cl、SO4和CaCO3的浓度比地下水高1.6 ~ 7.2倍。同样,硬度、碱度、电导率和总溶解固体也明显更高(增加了1.4到2.0倍)。这些结果表明,土壤和基岩正在将溶解成分淋滤到地下水中。McCallister湖的Ca (402 mg/L)、Na (1165 mg/L)、Cl (678 mg/L)、SO4 (3525 mg/L)和电导率(11,200 micromohs/cm)浓度升高,表明高蒸发使溶解盐浓度增加。持续的干旱条件将提高蒸发率,导致溶解盐和矿物质的积累增加,可能威胁湖泊生态系统的活力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
WATER QUALITY ASSESSMENT ALONG GALLINAS CREEK SURFACE WATER AND GROUNDWATER PATHWAYS, LAS VEGAS, NEW MEXICO
We report preliminary results of a pilot study that compared the chemistry of surface water and ground water within the Gallinas Watershed. Gallinas Creek originates in the southern Sangre de Cristo Mountains and flows southeast towards the high plains desert community of Las Vegas, New Mexico. A large percentage of flow is diverted to the Storrie Lake Water Project and divided among multiple users, including the city of Las Vegas, Las Vegas National Wildlife Refuge, and farmers and ranchers. We studied changes in water quality within different regions of the diverted water system. Samples were collected at four primary locations: the surface water source (Upper Gallinas River), diverted surface water (McCallister Lake), ground water seeps (springs along Gallinas Canyon) and ground water receptor (Lower Gallinas River). This study hypothesized that as water infiltrates through the subsurface, the area’s highly alkaline soils and the shallow bedrock aquifer contribute dissolved constituents to ground water. To test this hypothesis, surface water and ground water samples from Gallinas Creek sources were collected and analyzed for various water parameters. Our results indicate that Ca, Mg, Na, Si, Cl, SO4, and CaCO3 concentrations are 1.6 to 7.2 times higher in ground water. Likewise, hardness, alkalinity, conductivity, and total dissolved solids are also appreciably higher (increased by factor of 1.4 to 2.0). These results suggest that soils and bedrock are leaching dissolved constituents to ground water. McCallister Lake exhibits elevated Ca (402 mg/L), Na (1165 mg/L), Cl (678 mg/L), SO4 (3525 mg/L), and electrical conductivity (11,200 micromohs/cm) concentrations that suggest high evaporation is enriching dissolved salt concentrations. Continued drought conditions will enhance evaporation rates and lead to increasing accumulation of dissolved salts and minerals potentially threatening the vitality of the lake ecosystem.
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