Atmospheric S and N deposition relates to increasing riverine transport of S and N in southwest China: Implications for soil acidification
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文摘

The SO42− outflow flux from the Sichuan Basin is well-balanced with S deposition in the basin.

The increasing SO42− outflow in the Yangtze River implies regional soil acidification.

Nitrogen deposition currently contributes much less than S deposition to soil acidification.

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