Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.catena.2024.108012 |
Karst rocky desertification restoration increases soil inorganic N supply to reduce plant N limitation | |
Wen, Dongni; Huang, Yuanyuan; Huang, Yuanfei; Ding, Nana; Ni, Kang; Wang, Hua; Elrys, Ahmed S.; Meng, Lei; Zhu, Tongbin; Gessert, Alena; Mueller, Christoph | |
通讯作者 | Meng, L ; Zhu, TB |
来源期刊 | CATENA
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ISSN | 0341-8162 |
EISSN | 1872-6887 |
出版年 | 2024 |
卷号 | 241 |
英文摘要 | Nitrogen (N) limitation of plant growth following vegetation restoration is widespread in global terrestrial ecosystems, especially in karst rocky desertification areas. However, neither the temporal changes in plant N limitation during the restoration of those areas nor the mechanisms underlying N availability are well understood. In this study, several indicators reflecting soil N availability, N transformation rates, and plant communities were investigated in four areas in southwest China differing in their grade of rocky desertification. Our results showed that plant growth was severely N limited in the intense rocky desertification areas. The plant community-level foliar N content, N-15 values, and N:P ratio increased significantly as the rocky desertification grade decreased, indicating a decrease in plant N limitation. This was attributed to increased soil N availability, evidenced by the higher soil delta N-15 values as well as total N and inorganic N contents along the rocky desertification grade. With the decreasing rocky desertification grade, the rates of organic N conversion to ammonium (NH4+) and nitrate (NO3-), the adsorption of NH4+ on cation-exchange sites, and the release of adsorbed NH4+ increased significantly, which could enhance soil inorganic N supply capacity and accelerate NH4+ turnover to increase N availability. Noticeably, the sharp decrease in the rate of NH4+ oxidation to NO3- with the decrease in the rocky desertification grade led to a shift in inorganic N from NO3--dominated to NH4+-dominated. The increased contents of soil organic matter, calcium, iron-aluminum oxides, and sand, the proportion of aggregates > 2 mm, as well as the greater abundances of fungi and bacteria were the primary drivers of the N transformation rates along the rocky desertification grade. Overall, our study highlights the importance of N cycling in controlling N availability and thus in determining plant N limitation in karst rocky desertification areas. The results of the study provide a scientific basis for the ecological restoration of rocky desertification in karst ecosystems. |
英文关键词 | Rocky desertification Nitrogen availability Plant N limitation Gross N transformation rates Soil microbial community |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:001288178800001 |
WOS关键词 | CHINA KARST ; NITROGEN ; CARBON ; ECOSYSTEMS ; VEGETATION ; FUNGI |
WOS类目 | Geosciences, Multidisciplinary ; Soil Science ; Water Resources |
WOS研究方向 | Geology ; Agriculture ; Water Resources |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/403152 |
推荐引用方式 GB/T 7714 | Wen, Dongni,Huang, Yuanyuan,Huang, Yuanfei,et al. Karst rocky desertification restoration increases soil inorganic N supply to reduce plant N limitation[J],2024,241. |
APA | Wen, Dongni.,Huang, Yuanyuan.,Huang, Yuanfei.,Ding, Nana.,Ni, Kang.,...&Mueller, Christoph.(2024).Karst rocky desertification restoration increases soil inorganic N supply to reduce plant N limitation.CATENA,241. |
MLA | Wen, Dongni,et al."Karst rocky desertification restoration increases soil inorganic N supply to reduce plant N limitation".CATENA 241(2024). |
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