{"title":"The Rio Grande: Is the Past the Key to the Future?","authors":"F. Phillips","doi":"10.56577/sm-2013.68","DOIUrl":null,"url":null,"abstract":"The Rio Grande Valley receives the large majority of its water supply, both surface and ground water, from its headwaters in Colorado and northern New Mexico. This area constitutes a small fraction of the drainage basin. This hydrological reality imposes severe constraints on the potential supply of water for the inhabitants of the Rio Grande Valley. For most of its history, the inhabitants accommodated themselves to the flood-and-drought vagaries of the river, modifying it in only very minor ways. This changed with the incursion of railroads in New Mexico in the 1870's. The effects of access to distant markets and to modern engineering technology resulted in changes to the Rio Grande that, by the middle of the 20th century, made it scarcely recognizable as the same river that had existed 100 years prior. In many cases, the changes were not intentional, but rather arose from unforeseen outcomes of economic activities. We have now reached the point where water utilization is a zero-sum game. If water is to be put to new uses, it has to be taken away from an existing user. Water availability is the constraining limitation on human activity in the Rio Grande Valley. The question for the 21st century is whether the inhabitants of the Valley will continue to reallocate the water to satisfy blindly accepted societal goals, and suffer the inevitable unintended consequences, or whether they will recognize the limiting role of water supply and try to direct water use toward achieving the best quality of life possible within the water limitation.","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":null,"pages":null},"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-2013.68","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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Abstract

The Rio Grande Valley receives the large majority of its water supply, both surface and ground water, from its headwaters in Colorado and northern New Mexico. This area constitutes a small fraction of the drainage basin. This hydrological reality imposes severe constraints on the potential supply of water for the inhabitants of the Rio Grande Valley. For most of its history, the inhabitants accommodated themselves to the flood-and-drought vagaries of the river, modifying it in only very minor ways. This changed with the incursion of railroads in New Mexico in the 1870's. The effects of access to distant markets and to modern engineering technology resulted in changes to the Rio Grande that, by the middle of the 20th century, made it scarcely recognizable as the same river that had existed 100 years prior. In many cases, the changes were not intentional, but rather arose from unforeseen outcomes of economic activities. We have now reached the point where water utilization is a zero-sum game. If water is to be put to new uses, it has to be taken away from an existing user. Water availability is the constraining limitation on human activity in the Rio Grande Valley. The question for the 21st century is whether the inhabitants of the Valley will continue to reallocate the water to satisfy blindly accepted societal goals, and suffer the inevitable unintended consequences, or whether they will recognize the limiting role of water supply and try to direct water use toward achieving the best quality of life possible within the water limitation.
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格兰德河:过去是未来的关键吗?
里奥格兰德河谷的大部分水源,包括地表水和地下水,都来自其源头科罗拉多州和新墨西哥州北部。这个地区构成了流域的一小部分。这种水文现实严重限制了里奥格兰德河谷居民的潜在供水。在历史上的大部分时间里,居民们适应了河流变幻莫测的洪水和干旱,只是对它进行了非常微小的修改。这种情况随着1870年代铁路在新墨西哥州的入侵而改变。由于进入遥远的市场和现代工程技术的影响,格兰德河发生了变化,到20世纪中叶,人们几乎认不出它是100年前存在的那条河。在许多情况下,这些变化不是有意的,而是由经济活动的不可预见的结果引起的。我们现在已经到了用水是零和游戏的地步。如果要把水用于新的用途,就必须从现有用户那里取走。水的可用性是制约格兰德河流域人类活动的制约因素。21世纪的问题是,山谷的居民是否会继续重新分配水资源,以满足盲目接受的社会目标,并承受不可避免的意想不到的后果,或者他们是否会认识到供水的有限作用,并试图在水资源限制的范围内指导用水,以实现尽可能高的生活质量。
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