The Atacama Desert’s Hyperaridity Gradient and Lithium-Brine Extraction Zoning under Climate-Induced Aquifer Stress
阿塔卡马沙漠的极端干旱梯度与气候胁迫下卤水提锂开采空间分区
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The Atacama Desert hosts the world’s most intense hyperaridity gradient, spanning from 1 mm to 200 mm annual precipitation across just 150 km.
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This gradient directly controls the spatial distribution of lithium-rich brine aquifers beneath salars, whose recharge rates have declined by 37% since 2000.
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