在灌农业系统中,矿物土壤和沉积物从矿物土壤和沉积物释放出水溶性有机碳
Sandrine J Matiasek1, Brian A Pellerin2, Robert G M Spencer1
1Department of Land, Air and Water Resources, University of California, One Shields Avenue, Davis, CA 95616, USA.
Journal of environmental management
|May 27, 2023
概括
农业土壤将溶解有机碳 (DOC) 和沉积物释放到水中. 我们的研究量化了沉积物和土壤中的水溶性有机碳 (WSOC) 如何为DOC流提供贡献,发现它是一个重要的,尽管以前被低估的来源.
科学领域:
- 环境科学 环境科学
- 土壤科学 土壤科学
- 水文学的水文学
背景情况:
- 农业水域在水-土壤-植被相互作用方面与自然景观不同,影响有机碳 (OC) 循环.
- 耕作农业土壤缺乏有机地平线,导致矿物土壤将溶解有机碳 (DOC) 和沉积物释放到地表水中.
- 在灌流域,同时增加的DOC和总悬浮沉积物 (TSS) 表明与沉积物相关的OC是主要的DOC来源.
研究的目的:
- 量化来自沉积物和土壤的水溶性有机碳 (WSOC) 在农业流域的DOC流中的贡献.
- 为了确定来自农业沉积物和土壤的OC的溶解效率和潜力.
主要方法:
- 在悬浮和床沉积物以及来自加利福尼亚州灌农业流域的土壤上进行了无生物溶解实验.
- 在测试度范围内的沉积物和土壤中观察到线性溶解行为.
- 在灌季的悬浮沉积物中,溶解效率和溶解潜力最高.
主要成果:
- 在灌季节悬浮沉积物显示出最高的溶解效率 (10.9%) 和潜力 (1.79毫克WSOCg-1干沉积物).
- 连续的溶解使WSOC的总释放量增加了约50%,但大多数 (88-97%) 的固态OC仍然不溶.
- 据估计,悬浮沉积物中的WSOC占年度流域DOC出口量的4-7%.
结论:
- 沉积物相关的OC是农业河流,特别是灌系统中DOC的重要来源.
- 虽然悬浮沉积物的WSOC对DOC出口有可衡量的贡献,但沉积物的实际现场规模贡献可能要高得多.
- 需要进一步的研究才能充分理解沉积物OC在农业流域生物地质化学中的作用.
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