路易斯安那州卡多教区克罗斯湖水质和底质特征

B. McGee
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引用次数: 1

摘要

克罗斯湖是一个浅的、单一的湖泊,是在1926年由克罗斯河口的蓄水形成的。这个湖是路易斯安那州什里夫波特市的主要饮用水来源。近年来,湖岸日益城市化。此外,向克罗斯湖提供径流的流域的土地利用也发生了变化。土地利用和城市化的变化会影响湖泊的水化学和生物。在1997年2月至1999年2月期间,收集了克罗斯湖10个地点的水质数据。采集水柱和底料样品。水柱样本每年至少收集四次。分析的这些样品包括物理和化学相关性质,如水温、溶解氧、pH值和比电导;选定的主要无机离子;营养物质;次要的元素;有机化学成分;和细菌。在采样期间共采集了7次悬浮沉积物样品。取样期间采集一次底料样品,对选定的微量元素和无机碳进行分析。除营养状况良好外,整体水质较好。本报告分析的任何水质成分均未超过联邦或州的主要水质标准。除铁和锰外,主要无机成分浓度较低。湖水是一种碳酸氢钠类型的软水。微量元素和有机化合物的浓度很低,许多低于检测极限。氮和磷是出现在最高浓度的养分。营养物均匀分布在整个湖泊,没有特定的水质点表明营养物浓度持续升高或降低。分析的水样中硝酸盐含量没有超过美国环境保护署规定的每升10毫克的最大污染物水平。根据Cross Lake计算的氮磷比,所有水质点的中位数都在氮限制范围内(小于或等于5)。Cross Lake的历史营养状态指数将湖泊划分为富营养化。最近(1998-99)的营养状态指数将横湖划分为中营养化-富营养化,这可能表明富营养化的减少。沉积圈闭表明克罗斯湖以平均每年0.41英寸的速度填满。粪大肠菌群和链球菌的浓度普遍较低。粪便大肠菌群的检测浓度高于粪便链球菌。在降雨径流事件发生后不久,检测到高浓度的细菌,可能是将周围地区的细菌冲入湖中。
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 and bottom-material characteristics of Cross Lake, Caddo Parish, Louisiana, 1997-99
Cross Lake is a shallow, monomictic lake that was formed in 1926 by the impoundment of Cross Bayou. The lake is the primary drinking-water supply for the City of Shreveport, Louisiana. In recent years, the lakeshore has become increasingly urbanized. In addition, the land use of the watershed contributing runoff to Cross Lake has changed. Changes in land use and urbanization could affect the water chemistry and biology of the Lake. Water-quality data were collected at 10 sites on Cross Lake from February 1997 to February 1999. Water-column and bottom-material samples were collected. The water-column samples were collected at least four times per year. These samples analyzed included physical and chemical-related properties such as water temperature, dissolved oxygen, pH, and specific conductance; selected major inorganic ions; nutrients; minor elements; organic chemical constituents; and bacteria. Suspended-sediment samples were collected seven times during the sampling period. The bottom-material samples, which were collected once during the sampling period, were analyzed for selected minor elements and inorganic carbon. Aside from the nutrient-enriched condition of Cross Lake, the overall water-quality of Cross Lake is good. No primary Federal or State water-quality criteria were exceeded by any of the water-quality constituents analyzed for this report. Concentrations of major inorganic constituents, except iron and manganese, were low. Water from the lake is a sodium-bicarbonate type and is soft. Minor elements and organic compounds were present in low concentrations, many below detection limits. Nitrogen and phosphorus were the nutrients occurring in the highest concentrations. Nutrients were evenly distributed across the lake with no particular water-quality site indicating consistently higher or lower nutrient concentrations. No water samples analyzed for nitrate exceeded the U.S. Environmental Protection Agency’s Maximum Contaminant Level of 10 milligrams per liter. Based on nitrogen to phosphorus ratios calculated for Cross Lake, median values for all water-quality sites were within the nitrogen-limited range (less than or equal to 5). Historical Trophic State Indexes for Cross Lake classified the lake as eutrophic. Recent (1998-99) Trophic State Indexes classify Cross Lake as mesotrophic-eutrophic, which might indicate a reduction in eutrophication. Sedimentation traps indicate that Cross Lake is filling at an average rate of 0.41 inch per year. Concentrations of fecal-coliform and streptococci bacteria generally were low. Fecal coliform was detected in higher concentrations than fecal streptococci. High bacteria concentrations were measured shortly after rainfall-runoff events, possibly washing bacteria from surrounding areas into the lake.
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