Analysis of streamflow and water-quality data at two long-term monitoring sites on the St. Croix River, Wisconsin and Minnesota

Bernard N. Lenz
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引用次数: 3

Abstract

Streamflow of the St. Croix River has been monitored on a long-term basis by the U.S. Geological Survey (USGS) at streamflow-gaging stations on the St. Croix River at Wisconsin State Highway 35 near Danbury, Wisconsin and below the dam at St. Croix Falls, Wisconsin. Trend analysis indicates that annual streamflow peaks, annual mean flows, and annual 7-day low flows have remained relatively stable at the Danbury (upstream) station from 1914 to 2001 but have increased by 0.45 to 0.55 percent per year at the St. Croix Falls (downstream) station from 1902 to 2001. Water-quality sampling conducted by the USGS at two associated water-quality monitoring sites from 1964 to 2001 have included analysis for nutrients, suspended sediments, metals, bacteria, and pesticides. The water-quality data at the two sites had considerable temporal variation and was often limited in extent by the data-collection needs of previous projects. The absence of consistent long-term water-quality data made detection of statistically significant trends in the water-quality data difficult. Nutrient, suspended-sediment, and major ion concentrations and field parameters were generally higher and more variable at the St. Croix Falls site than at the Danbury site. However, disparate sampling periods and strategies could cause possible biases in the comparison of water quality between sites. Introduction The U.S. Geological Survey (USGS) has performed long-term continuous streamflow measurements of the St. Croix River at two streamflow-gaging stations: at Wisconsin State Highway 35 near Danbury, Wisconsin and below the dam at St. Croix Falls, Wisconsin (fig. 1). Water-quality measurements of a variety of constituents such as nutrients, suspended sediments, metals, bacteria, and pesticides have been collected at two water-quality monitoring sites associated with these streamflow-gaging stations. This report will refer to both the streamflow-gaging stations and associated water-quality monitoring sites as sites. This study, which was initiated in 2001, was a cooperative effort between the USGS, National Park Service (NPS), and the Joint Water Quality Commission of Danbury and St. Croix Chippewa Indians of Wisconsin to analyze the long-term USGS flow data for temporal trends and provide summaries and analysis of the USGS water-quality data collected at these sites. This report presents trends in flow and differences in water quality among sites, studies, and over time. Streamflow data from 1902 to 2001 and water-quality data from 1964 to 2001 are included in this study. Differences between the long-term data sets can be used to determine the part of the St. Croix River Basin where change has occurred. Trends at the Danbury site reflect changes in the upper basin (1,580 square miles), trends in the difference between the St. Croix Falls and Danbury sites reflect changes that occurred in the part of the drainage basin between those two sites (4,660 square miles), and trends at the St. Croix Falls EXPLANATION M I N N E S O T A
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对威斯康星州和明尼苏达州圣克罗伊河两个长期监测点的流量和水质数据进行分析
美国地质调查局(USGS)在位于威斯康星州丹伯里附近的威斯康星州35号高速公路上的圣克罗伊河流量测量站和威斯康星州圣克罗伊瀑布大坝下方的流量测量站对圣克罗伊河的流量进行了长期监测。趋势分析表明,1914年至2001年,Danbury(上游)站的年流量峰值、年平均流量和年7日低流量保持相对稳定,而St. Croix Falls(下游)站的年流量峰值、年平均流量和年7日低流量在1902年至2001年期间每年增加0.45%至0.55%。从1964年到2001年,美国地质调查局在两个相关的水质监测点进行了水质采样,包括对营养物质、悬浮沉积物、金属、细菌和杀虫剂的分析。这两个地点的水质数据在时间上有很大的变化,而且往往受到以往项目收集数据需要的限制。由于缺乏一致的长期水质数据,很难发现水质数据中具有统计意义的趋势。与丹伯里遗址相比,圣克罗伊瀑布遗址的营养物质、悬浮沉积物、主要离子浓度和野外参数普遍更高,变化也更大。然而,不同的采样周期和策略可能会导致不同地点之间水质比较的可能偏差。美国地质调查局(USGS)在两个流量测量站对圣克罗伊河进行了长期连续的流量测量:在威斯康星州丹伯里附近的威斯康星州35号高速公路和威斯康星州圣克罗伊瀑布的大坝下方(图1)。在与这些流量测量站相关的两个水质监测点收集了各种成分的水质测量数据,如营养物质、悬浮沉积物、金属、细菌和农药。本报告将把流量测量站和相关的水质监测点都称为监测点。这项研究始于2001年,是美国地质勘探局、国家公园管理局(NPS)和威斯康星州丹伯里和圣克罗伊奇佩瓦印第安人联合水质委员会之间的一项合作,目的是分析美国地质勘探局的长期流量数据的时间趋势,并提供美国地质勘探局在这些地点收集的水质数据的摘要和分析。本报告介绍了不同地点、不同研究和不同时期的水流趋势和水质差异。本文采用了1902 ~ 2001年的河流流量数据和1964 ~ 2001年的水质数据。长期数据集之间的差异可以用来确定圣克罗伊河流域发生变化的部分。丹伯里遗址的趋势反映了上游盆地(1580平方英里)的变化,圣克罗伊瀑布和丹伯里遗址之间差异的趋势反映了这两个遗址之间部分流域盆地(4660平方英里)的变化,以及圣克罗伊瀑布的趋势
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