水平衡在全球范围内创造了土壤pH值的门
E W Slessarev1, Y Lin2, N L Bingham3
1Department of Ecology, Evolution, and Marine Biology, University of California, Santa Barbara, California, USA.
Nature
|November 22, 2016
概括
当降水超过蒸发时,全球土壤的pH从性过渡到酸性. 这一气候驱动的门影响了全球的土壤肥力和营养.
科学领域:
- 环境科学
- 土壤科学
- 生态学
背景情况:
- 土壤pH对于营养储存,供应和陆地生态系统的生产力至关重要.
- 土壤的pH主要由环境因素控制,特别是水平衡.
- 之前对土壤pH值的理解受限于地形和矿物学等因素.
研究的目的:
- 在全球量化水平衡和土壤pH之间的关系.
- 确定土壤pH从性转变为酸性的关键值.
- 调查导致全球土壤pH值偏差的因素.
主要方法:
- 使用了60,291个土壤pH测量的全球数据集.
- 抽取了2万个测量的随机样本进行分析.
- 相关的土壤pH与年平均降水和潜在的蒸发.
主要成果:
- 发现了从性土壤到酸性土壤的突然转变.
- 这种过渡发生在平均年降水量超过平均年潜在蒸发量时.
- 季节性,气候历史,侵蚀和矿物学解释了全球模式的偏差.
结论:
- 气候是全球土壤溶液化学的主要驱动因素,产生非线性pH模式.
- 这项研究揭示了土壤pH值可能与现代气候不均衡的情况.
- 了解这一门对于预测土壤肥力和生态系统对气候变化的反应至关重要.
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