4.7 Article

The Contribution of Anammox to Nitrogen Removal Is Greater in Bulk Soils Than in Rhizosphere Soils in Riparian Wetlands Along the Yangtze River

期刊

GLOBAL BIOGEOCHEMICAL CYCLES
卷 37, 期 5, 页码 -

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2022GB007576

关键词

bulk soils; denitrification; microbial abundance; nitrogen cycling; Yangtze River

向作者/读者索取更多资源

This study demonstrates that denitrification and anammox rates are significantly higher in rhizosphere soils compared to bulk soils, indicating that the rhizosphere environment is favorable for nitrogen removal. Anammox constitutes over half of the nitrogen loss, with higher rates observed in bulk soils than in rhizosphere soils. Therefore, revegetation can effectively enhance the nitrogen removal function of riparian wetlands along the Yangtze River.
The importance of denitrification and anaerobic ammonium oxidation (anammox) in removing nitrogen (N) from upland runoff has been well documented in riparian wetlands. However, the relative contributions of denitrification and anammox to N removal in the rhizosphere and non-rhizosphere soils of riparian zones remain unclear. Here, we explored the denitrification and anammox rates in the rhizosphere and bulk soils (0-5 and 10-15 cm) of 39 riparian wetlands along the Yangtze River using the 15N isotope pairing technique. Additionally, we used a quantitative polymerase chain reaction assay to determine the abundance of soil denitrifying and anammox bacteria using nosZ and hzsB genes, respectively. The results showed that both denitrification and anammox rates were significantly higher in rhizosphere soils than in bulk soils, suggesting that the rhizosphere environment is favorable for N removal. The contribution of anammox constituted over half (62.53% +/- 1.49%) of the N loss and was greater in bulk soils (68.57% +/- 1.42%) than in rhizosphere soils (55.64% +/- 2.42%). Higher nosZ and hzsB gene abundances were also observed in rhizosphere soils than in bulk soils. Denitrification and anammox rates were significantly regulated by edaphic properties, microbial abundance, and plant biomass. The structural equation model further revealed that soil pH and N availability could affect denitrification and anammox rates both directly and indirectly by altering nosZ and hzsB gene abundance. Overall, this study highlights that the rhizosphere is a control point for N removal and harbors more functional microbes than bulk soils. Therefore, revegetation may effectively enhance the N removal function of riparian wetlands along the Yangtze River.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据