首页> 外文OA文献 >Temperature change affected groundwater quality in a confined marine aquifer during long-term heating and cooling

【2h】

Temperature change affected groundwater quality in a confined marine aquifer during long-term heating and cooling

机译：在长期供暖和制冷期间，温度变化会影响承压海水含水层的地下水水质

代理获取

本网站仅为用户提供外文OA文献查询和代理获取服务，本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文，但由于OA文献来源多样且变更频繁，仍可能出现获取不到、文献不完整或与标题不符等情况，如果获取不到我们将提供退款服务。请知悉。

页面导航

摘要
著录项
相似文献
相关主题

摘要

Highlights•Effect of subsurface temperature change on groundwater quality was investigated.•Concentration of several components increased linearly with increase in temperature.•Boron concentration increased by 31% with increase in temperature of 7 °C.•Elevated concentrations returned to original levels with decrease in temperature.

机译：要点•研究了地下温度变化对地下水水质的影响。•随着温度的升高，几种组分的浓度呈线性增加。•随着温度升高7°C，硼的浓度增加了31％。•升高的浓度随着温度的降低而恢复到原始水平温度。

著录项

作者
Saito, Takeshi; Hamamoto, Shoichiro; Ueki, Takashi; Ohkubo, Satoshi; Møldrup, Per; Kawamoto, Ken; Komatsu, Toshiko;
展开▼
作者单位

展开▼
年度 2016
总页数
原文格式 PDF
正文语种 eng
中图分类

相似文献

外文文献
中文文献
专利

1. Temperature change affected groundwater quality in a confined marine aquifer during long-term heating and cooling [J] . Saito Takeshi, Hamamoto Shoichiro, Ueki Takashi, Water Research . 2016,第May1期

机译：在长期加热和冷却期间，温度变化影响了受限海洋含水层中的地下水质量
2. Statistical and numerical analyses of the influence of climate variability on aquifer water levels and groundwater temperatures: The impacts of climate change on aquifer thermal regimes [J] . Luminda Niroshana Gunawardhana, So Kazama Global and planetary change . 2012,第Apra期

机译：气候变化对含水层水位和地下水温度影响的统计和数值分析：气候变化对含水层热力状态的影响
3. Long-term groundwater dynamics in the coastal confined aquifers of Venice (Italy) [J] . Cristina Da Lio, Luigi Tosi, Giuseppe Zambon, Estuarine Coastal and Shelf Science . 2013,第deca20期

机译：威尼斯（意大利）沿海承压含水层中的长期地下水动力学
4. Geochemical Modelling of Groundwater Quality Changes during Aquifer Storage and Recovery (ASR) in the dual porosity Chalk aquifer, England [C] . I.Gaus, P.Shand, I.N.Gale, Water-Rock Interaction . 2001

机译：英格兰双重孔隙白垩含水层中含水层储存和恢复（ASR）过程中地下水质量变化的地球化学模拟
5. The effects of past climate change and recent agricultural irrigation recharge on the sources, ages, and quality of groundwater in the Columbia River Basalt Aquifers, Columbia Basin, Central Washington. [D] . Brown, Kyle. 2009

机译：华盛顿中部哥伦比亚盆地哥伦比亚河玄武岩含水层中，过去的气候变化和最近的农业灌溉补给对地下水的来源，年龄和质量的影响。
6. Preseismic Changes of the Level and Temperature of Confined Groundwater related to the 2011 Tohoku Earthquake [O] . Yoshiaki Orihara, Masashi Kamogawa, Toshiyasu Nagao -1

机译：与2011年东北地震有关的承压地下水位和温度的地震变化
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。

Temperature change affected groundwater quality in a confined marine aquifer during long-term heating and cooling

摘要

著录项

相似文献

相关主题

期刊订阅