气候变化领域集成服务门户(CCPortal): Carbon persistence of soils with long-term biosolids amendments in California agroecosystems

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DOI	10.1002/saj2.20632
	Carbon persistence of soils with long-term biosolids amendments in California agroecosystems
	Villa, Yocelyn B.; Phosalath, Eddie; Ryals, Rebecca
发表日期	2024
ISSN	0361-5995
EISSN	1435-0661
起始页码	88
结束页码	2
卷号	88 期号:2
英文摘要	Biosolids can build soil organic matter, but their ability to increase carbon and nitrogen in persistent fractions in deep soil is not well understood. We aimed to assess the mechanisms that influence soil carbon and nitrogen dynamics at three sites-Sacramento (irrigated, grazed grassland), Solano (rainfed, grazed grassland), and Merced (feed cropping system with alfalfa-corn rotation)-where soils were amended with biosolids for 20 years using density fractionations, organomineral extractions, and correlations between calcium and soil organic carbon at three depths (0-10, 30-50, and 75-100 cm). We found that amended soils had higher carbon and nitrogen content in the free- and occluded-light fractions at all depths relative to the control in the Sacramento and Solano sites; however, the Merced site had a greater relative increase of carbon and nitrogen associated with the heavy fraction. Effect sizes show that biosolids increase carbon and nitrogen content in free- and occluded-light fractions in the surface soil (0-10 cm), and in both light and heavy fractions in the deep soil layer (75-100 cm). Ratios of carbon to iron and aluminum show that chelation is an important mechanism of carbon stabilization in Sacramento and Solano sites throughout the soil profile. No (0-10 cm) to negative (75-100 cm) correlations were observed between calcium and soil carbon in the amended soils in the Merced site. Our results indicate that, while biosolids are typically incorporated at shallow depths, long-term application of biosolids can increase the amount of free- and occluded-light carbon fractions in deep soil. Long-term biosolids increased deep soil C and N concentrations. Density fractionation indicates amended soils had more labile C and N in surface soils. Organometal complexes were a stabilization mechanism in two of the three sites. Negative correlations between C and Ca2+ in amended soils indicate biosolids interact with C. Accounting for deep soil C demonstrated the importance of assessing the climate change mitigation potential of managed soil.
语种	英语
WOS研究方向	Agriculture
WOS类目	Soil Science
WOS记录号	WOS:001161989900001
来源期刊	SOIL SCIENCE SOCIETY OF AMERICA JOURNAL
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/304152
作者单位	University of California System; University of California Merced; University of California System; University of California Merced; University of California System; University of California Merced
推荐引用方式 GB/T 7714	Villa, Yocelyn B.,Phosalath, Eddie,Ryals, Rebecca. Carbon persistence of soils with long-term biosolids amendments in California agroecosystems[J],2024,88(2).
APA	Villa, Yocelyn B.,Phosalath, Eddie,&Ryals, Rebecca.(2024).Carbon persistence of soils with long-term biosolids amendments in California agroecosystems.SOIL SCIENCE SOCIETY OF AMERICA JOURNAL,88(2).
MLA	Villa, Yocelyn B.,et al."Carbon persistence of soils with long-term biosolids amendments in California agroecosystems".SOIL SCIENCE SOCIETY OF AMERICA JOURNAL 88.2(2024).