从土壤到海洋的有机碳酸盐关系的固体测量控制
Philip G Taylor1, Alan R Townsend
1INSTAAR, University of Colorado, Boulder, Colorado, USA. philip.taylor@colorado.edu
Nature
|April 24, 2010
概括
人类活动增加的活性会导致生态系统中酸盐的积累. 有机碳的可用性,由微生物过程和资源石化学驱动,控制了从土壤到海洋的各种环境中的酸盐水平.
科学领域:
- 环境科学 环境科学
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
背景情况:
- 人类的活动,如使用肥料,增加了活性,扰乱了全球循环.
- 在淡水和海洋生态系统中酸盐的积累是一个重大的环境问题.
- 循环的重组会影响粮食生产和生态系统的健康.
研究的目的:
- 研究生态系统酸盐积累和有机碳可用性之间的关系.
- 了解资源固体测量如何影响各种环境中的酸盐积累.
- 探索微生物过程在调节酸盐水平中的作用.
主要方法:
- 在水文连续 (土壤到开放的海洋) 上分析酸盐积累.
- 微生物过程合溶解的有机碳和酸盐循环的元分析.
- 检查资源固体几何学 (有机碳:酸盐比率) 以及其对微生物合成和代谢的影响.
主要成果:
- 生态系统酸盐积累显示了与有机碳可用性的负非线性相关性.
- 资源石化学 (有机碳:酸盐) 调节影响酸盐积累的微生物过程.
- 微生物过程,包括异质变异,化和脱化,在一个受约束的固态度窗口内运行.
结论:
- 生态固体测量为了解不同生态系统中酸盐命运提供了一个框架.
- 微生物对碳和循环的调节是控制酸盐积累的关键.
- 这些发现适用于自然环境和人为环境,为污染管理提供了洞察力.
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