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Pesticide Mixtures in the Sacramento–San Joaquin Delta, 2016–17: Results from Year 2 of the Delta Regional Monitoring Program 2016 - 2017年萨克拉门托-圣华金三角洲农药混合物:三角洲区域监测计划第二年的结果
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/ds1120
Matthew De Parsia, Emily E. Woodward, J. Orlando, M. Hladik
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引用次数: 2
Least Bell’s Vireo (Vireo bellii pusillus) and Southwestern Willow Flycatcher (Empidonax traillii extimus) surveys in the Sepulveda Dam Basin, Los Angeles County, California—2018 data summary 在加州洛杉矶县Sepulveda大坝盆地进行的Least Bell的Vireo (Vireo bellii pusillus)和西南捕蝇柳(emidonax traillii extimus)调查- 2018年数据摘要
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/ds1105
R. Pottinger, B. Kus
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引用次数: 0
Digital database of the geologic map of the middle east rift geothermal subzone, Kīlauea Volcano, Hawai‘i 夏威夷k<e:1>劳厄火山中东裂谷地热亚带地质图数字数据库
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/DS1111
M. Zoeller, F. Trusdell, Richard B. Moore
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引用次数: 0
Alaska Geochemical Database Version 3.0 (AGDB3)—Including “Best Value” Data Compilations for Rock, Sediment, Soil, Mineral, and Concentrate Sample Media 阿拉斯加地球化学数据库3.0版(AGDB3) -包括岩石,沉积物,土壤,矿物和浓缩样品介质的“最佳价值”数据汇编
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/ds1117
M. Granitto, Bronwen Wang, N. Shew, S. Karl, K. Labay, M. Werdon, S. Seitz, J. E. Hoppe
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引用次数: 3
Quality of surface water in Missouri, water year 2018 2018年密苏里州地表水质量
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/ds1119
R. Kay
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引用次数: 0
Regional hydraulic geometry characteristics of stream channels in the Ouachita Mountains of Arkansas 阿肯色瓦希托山脉河道的区域水力几何特征
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/ds1104
A. L. Pugh, R. Redman
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引用次数: 1
Abundance and productivity of marbled murrelets (Brachyramphus marmoratus) off central California during the 2018 breeding season 2018年繁殖季节加利福尼亚中部大理石纹小鱼(Brachyramphus marmoratus)的丰度和生产力
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/DS1107
J. Felis, Emily C. Kelsey, Josh Adams
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引用次数: 2
Catalog of earthquake parameters and description of seismograph and infrasound stations at Alaskan volcanoes—January 1, 2013, through December 31, 2017 2013年1月1日至2017年12月31日,阿拉斯加火山地震参数目录和地震仪和次声站描述
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/DS1115
J. P. Dixon, S. D. Stihler, M. Haney, J. Lyons, D. M. Ketner, K. Mulliken, T. Parker, J. Power
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引用次数: 12
Petrographic, geochemical, and geochronologic data for cenozoic volcanic rocks of the Tonopah, Divide, and Goldfield Mining Districts, Nevada 内华达州托诺帕、迪格和金矿区新生代火山岩的岩石学、地球化学和地质年代学资料
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/DS1099
E. A. du Bray, D. John, Peter A. Vikre, J. Colgan, M. Cosca, L. Morgan, R. Fleck, W. Premo, C. Holm-Denoma
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引用次数: 0
Water-level data for the Albuquerque Basin and adjacent areas, central New Mexico, period of record through September 30, 2017 截至2017年9月30日,新墨西哥州中部阿尔伯克基盆地及邻近地区的水位数据
Q4 Environmental Science Pub Date : 2019-01-01 DOI: 10.3133/ds1113
J. E. Beman, A. Ritchie, A. Galanter
The Albuquerque Basin, located in central New Mexico, is about 100 miles long and 25–40 miles wide. The basin is hydrologically defined as the extent of consolidated and unconsolidated deposits of Tertiary and Quaternary age that encompasses the structural Rio Grande Rift between San Acacia to the south and Cochiti Lake to the north. A 20-percent population increase in the basin from 1990 to 2000 and a 22-percent population increase from 2000 to 2010 resulted in an increased demand for water in areas within the basin. Drinking-water supplies throughout the basin were obtained solely from groundwater resources until December 2008, when the Albuquerque Bernalillo County Water Utility Authority (ABCWUA) began treatment and distribution of surface water from the Rio Grande through the San JuanChama Drinking Water Project. An initial network of wells was established by the U.S. Geological Survey (USGS) in cooperation with the City of Albuquerque from April 1982 through September 1983 to monitor changes in groundwater levels throughout the Albuquerque Basin. In 1983, this network consisted of 6 wells with analog-to-digital recorders and 27 wells where water levels were measured monthly. The network currently (2017) consists of 122 wells and piezometers. (A piezometer is a specialized well open to a specific depth in the aquifer, often of small diameter and nested with other piezometers open to different depths.) The USGS, in cooperation with the ABCWUA and the New Mexico Office of the State Engineer, currently (2017) measures and reports water levels from the 122 wells and piezometers in the network; this report presents water-level data collected by USGS personnel at those 122 sites through water years 2016 and 2017 (October 1, 2015, through September 30, 2017). Water levels that were collected from wells in previous water years were published in previous USGS reports. Introduction The Albuquerque Basin, located in central New Mexico, is about 100 miles long and 25–40 miles wide (fig. 1). The basin is defined as the extent of consolidated and unconsolidated deposits of Tertiary and Quaternary age that encompasses the structural Rio Grande Rift within the basin (Thorn and others, 1993). The basin is approximately bisected by the southward-flowing Rio Grande, the only perennial stream extending through the length of it. The study area, which includes the Albuquerque Basin and adjacent areas, extends from just upstream of Cochiti Lake south to San Acacia and from Tijeras Canyon west to near the intersection of Interstate 40 and the Bernalillo-Cibola County line. In 2000, the population of the Albuquerque Basin was about 690,000 (Bartolino and Cole, 2002). According to 2010 U.S. Census Bureau data, the 2010 population was about 840,000 (U.S. Census Bureau, 2011; calculated as sum of population for census tract centers within the basin). The basin population increased about 20 percent from 1990 to 2000 (Thorn and others, 1993; Bartolino and Cole, 2002) and
阿尔伯克基盆地位于新墨西哥州中部,长约100英里,宽25-40英里。该盆地在水文学上被定义为第三纪和第四纪固结和松散沉积的范围,包括南部的圣阿卡西亚和北部的科奇蒂湖之间的构造大裂谷。从1990年到2000年,流域人口增长了20%,从2000年到2010年,人口增长了22%,导致流域内地区对水的需求增加。直到2008年12月,整个盆地的饮用水供应完全来自地下水资源,当时阿尔伯克基伯纳利略县水务局(ABCWUA)开始通过圣胡安查马饮用水项目处理和分配来自里约热内卢格兰德的地表水。1982年4月至1983年9月,美国地质调查局(USGS)与阿尔伯克基市合作建立了一个初步的水井网络,以监测整个阿尔伯克基盆地地下水位的变化。1983年,该网络由6口装有模拟-数字记录仪的井和27口每月测量水位的井组成。该网络目前(2017年)由122口井和压电计组成。(压力计是在含水层中向特定深度打开的专用井,通常直径较小,并与其他打开不同深度的压力计嵌套在一起。)美国地质勘探局与ABCWUA和新墨西哥州国家工程师办公室合作,目前(2017年)测量并报告网络中122口井和压力表的水位;本报告展示了美国地质勘探局人员在2016年和2017年(2015年10月1日至2017年9月30日)期间在这122个地点收集的水位数据。在以前的水年里从井中收集的水位在以前的美国地质勘探局报告中公布。阿尔伯克基盆地位于新墨西哥州中部,长约100英里,宽约25-40英里(图1)。该盆地被定义为第三纪和第四纪固结和未固结沉积的范围,包括盆地内的构造里约热内卢大裂谷(Thorn等人,1993)。盆地大约被向南流动的里约热内卢Grande一分为二,这是唯一一条贯穿整个盆地的多年生河流。研究区域包括Albuquerque盆地和邻近地区,从Cochiti湖的上游向南延伸到San Acacia,从Tijeras峡谷向西延伸到40号州际公路和Bernalillo-Cibola县线的交汇处。2000年,阿尔伯克基盆地的人口约为69万(Bartolino and Cole, 2002)。根据2010年美国人口普查局的数据,2010年人口约为84万(美国人口普查局,2011;按流域内人口普查区中心的人口总数计算)。从1990年到2000年,流域人口增加了约20% (Thorn等人,1993;Bartolino和Cole, 2002年),2000年至2010年约为22%(美国人口普查局,2011年)。大部分人口集中在阿尔伯克基的城市范围内,2000年人口为448,607人,2010年人口为545,852人(美国人口普查局,2012)。在2008年之前,由于整个阿尔伯克基盆地的饮用水供应完全来自地下水资源,对地下水的需求随着人口的增加而增加。2008年12月,阿尔伯克基伯纳利略县水务局(ABCWUA)开始通过圣胡安-查马饮用水项目处理和分配来自里约热内卢Grande的地表水给他们的客户。2新墨西哥州中部阿尔伯克基盆地及邻近地区的水位数据,记录期至2017年9月30日laf18-0871_fig 01 40 25
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引用次数: 1
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U.S. Geological Survey Data Series
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