{"title":"新墨西哥州Jemez河沿岸砷浓度和理化参数的日波动","authors":"L. Garcia, Daryl J. Williams, E. Martinez","doi":"10.56577/sm-2013.87","DOIUrl":null,"url":null,"abstract":"Snow pack dominated rivers and streams across the Southwestern United States have been feeling the effects of global climate change, which mainly include increasing temperatures and decreasing amounts of precipitation, especially precipitation in the form of snow. Over the past 50 years the Jemez River regions has experienced a 2oF increase in ambient air temperature, as well as a 40% decrease in stream discharge. Spanning roughly 129 km and contributing more than 50,000,000 cubic meters of water to the Rio Grande River annually, the Jemez River is the largest tributary to the Middle Rio Grande Basin. Further complicating matters, the surrounding geology of the Jemez River is of volcanic origin which is responsible for the many hydrothermal springs and seeps in the area, which allow for","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"6 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Diurnal Fluctuations of Arsenic Concentrations and Physiochemical Parameters along the Jemez River, New Mexico\",\"authors\":\"L. Garcia, Daryl J. Williams, E. Martinez\",\"doi\":\"10.56577/sm-2013.87\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Snow pack dominated rivers and streams across the Southwestern United States have been feeling the effects of global climate change, which mainly include increasing temperatures and decreasing amounts of precipitation, especially precipitation in the form of snow. Over the past 50 years the Jemez River regions has experienced a 2oF increase in ambient air temperature, as well as a 40% decrease in stream discharge. Spanning roughly 129 km and contributing more than 50,000,000 cubic meters of water to the Rio Grande River annually, the Jemez River is the largest tributary to the Middle Rio Grande Basin. Further complicating matters, the surrounding geology of the Jemez River is of volcanic origin which is responsible for the many hydrothermal springs and seeps in the area, which allow for\",\"PeriodicalId\":363585,\"journal\":{\"name\":\"Proceedings Volume: \\\"Hydrology and History of the Rio Grande\\\", New Mexico Geological Society, 2013 Annual Spring Meeting\",\"volume\":\"6 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2013-04-12\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Proceedings Volume: \\\"Hydrology and History of the Rio Grande\\\", New Mexico Geological Society, 2013 Annual Spring Meeting\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.56577/sm-2013.87\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.56577/sm-2013.87","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Diurnal Fluctuations of Arsenic Concentrations and Physiochemical Parameters along the Jemez River, New Mexico
Snow pack dominated rivers and streams across the Southwestern United States have been feeling the effects of global climate change, which mainly include increasing temperatures and decreasing amounts of precipitation, especially precipitation in the form of snow. Over the past 50 years the Jemez River regions has experienced a 2oF increase in ambient air temperature, as well as a 40% decrease in stream discharge. Spanning roughly 129 km and contributing more than 50,000,000 cubic meters of water to the Rio Grande River annually, the Jemez River is the largest tributary to the Middle Rio Grande Basin. Further complicating matters, the surrounding geology of the Jemez River is of volcanic origin which is responsible for the many hydrothermal springs and seeps in the area, which allow for