原文服务方: 地球化学学报(英文)       
摘要:
One of the greatest challenges in critical zone studies is to document the moisture dynamics, water flux, and solute chemistry of the unsaturated, fractured and weathered bedrock that lies between the soil and groundwater table. The central impediment to quantifying this component of the subsurface is the difficulty associated with direct observations. Here, we report solute chemistry as a function of depth collected over a full year across the shale-derived vadose zone of the Eel River Critical Zone Observatory using a set of novel sub-horizontal wellbores, referred to as the vadose zone monitoring system. The results of this first geochemical glimpse into the deep vadose zone indicate a dynamic temporal and depth-resolved structure. Major cation concentrations reflect seasonal changes in precipitation and water saturation, and normalized ratios span the full range of values reported for the world's largest rivers.
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篇名 Seasonal shifts in the solute ion ratios of vadose zone rock moisture from the Eel River Critical Zo
来源期刊 学科 地球科学
关键词 Vadose zone Solute ion ratios Critical Zone Observatory Seasonal solute dynamics
年,卷(期) 2022,(3) 所属期刊栏目
研究方向 页码范围 385-388
页数 3页 分类号
字数 语种 英文
DOI 10.1007/s11631-017-0169-z
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Vadose zone
Solute ion ratios
Critical Zone Observatory
Seasonal solute dynamics
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地球化学学报(英文)
双月刊
2096-0956
52-1161/p
16开
贵阳市林城西路99号
1982-01-01
英语
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230
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