通过在亚马逊流域的地表土壤过程控制溪流水中的阴离子度
D Markewitz1, E A Davidson, Figueiredo Rd
1The Woods Hole Research Center, Woods Hole, Massachusetts 02543, USA. dmarke@smokey.forestry.uga.edu
Nature
|April 12, 2001
概括
在亚马逊极度受天气影响的土壤中,溪水化学是由表面土壤冲洗控制的,而不是深层气候. 森林燃烧丰富了土壤,通过生物介导的离子出,支持未来的森林再生.
科学领域:
- 地质化学 地质化学
- 热带土壤科学 热带土壤科学
- 水文学的水文学
背景情况:
- 温带生态系统中的水化学主要由岩石气候变化驱动.
- 了解古老的热带土壤中的水化学是有限的.
- 主要矿物质通过碳酸溶解是温带土壤的关键.
研究的目的:
- 调查在亚马逊极度受天气影响的流水流域中流水化学的驱动因素.
- 在热带与温带土壤中比较气候变化和浸出过程.
- 评估过去森林燃烧对土壤质可用性的长期影响.
主要方法:
- 从1万公的巴西亚马逊流域收集和分析了土壤和水化学数据.
- 与排放相关的溪水阴离子度和性.
- 检查了水化学中的季节性模式.
主要成果:
- 流水中的阴离子度和度与排放呈正相关,表明表面冲洗.
- 观察到的模式不同于温带生态系统,这表明不同的气候控制.
- 过去的森林燃烧丰富了土壤,可能会增加雨季的阴离子出.
结论:
- 在这种高度受天气影响的土壤流域中,流水的化学成分主要由表面土壤冲洗控制,由生物介导的二氧化碳生产驱动.
- 每年的阳离子输入和输出是平衡的,确保阳离子可用于未来的森林再生.
- 这些发现与温带生态系统形成鲜明对比,突出了独特的热带土壤水文过程.
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