由于气候变化,大陆范围的土壤透性可能会加剧水循环
Daniel R Hirmas1, Daniel Giménez2, Attila Nemes3
1Department of Environmental Sciences, University of California, Riverside, CA, USA. daniel.hirmas@ucr.edu.
Nature
|September 7, 2018
概括
干燥的气候会产生更多的土壤透性, 这些土壤变化可以显著改变水的导电性,影响气候反.
科学领域:
- 土壤科学
- 水文学
- 气候科学
背景情况:
- 土壤巨孔对于水的透,营养物质的运输和排水至关重要.
- 虽然巨孔的体积很小,但它们对水的流动和全球水循环有着不成比例的影响.
- 气候影响土壤巨孔的发展,但这些影响的速度和规模尚不清楚.
研究的目的:
- 研究气候和土壤透性之间的关系.
- 确定土壤透性因气候变化的时间表.
- 预测未来气候变化对土壤水力性能的影响.
主要方法:
- 分析了气候 (降水) 和土壤透性之间的相关性.
- 使用有效的多孔性作为巨大的多孔性.
- 基于预测降水变化的和土壤液压导电性的模型变化.
主要成果:
- 与潮湿气候相比,干燥气候导致土壤透性更大.
- 气候诱导的宏性变化发生在几年到几十年内,比以前假设的更快.
- 预计本世纪末降水变化可能会改变美国各地区和土壤的液压导电率 -55%至34%.
结论:
- 土壤透性对快速气候变化很敏感.
- 由于气候变化而改变的土壤液压特性可能会产生重大陆地表面反.
- 这些反可能会加剧大陆范围的水循环.
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