Nitrogen deposition impacts on the amount and stability of soil organic matter in an alpine meadow ecosystem depend on the form and rate of applied nitrogen
文献类型：期刊论文
| 作者 | Fang, H. J. ; Cheng, S. L. ; Yu, G. R. ; Yang, X. M. ; Xu, M. J. ; Wang, Y. S. ; Li, L. S. ; Dang, X. S. ; Wang, L. ; Li, Y. N. |
| 刊名 | EUROPEAN JOURNAL OF SOIL SCIENCE
 ; Fang, HJ; Cheng, SL; Yu, GR; Yang, XM; Xu, MJ; Wang, YS; Li, LS; Dang, XS; Wang, L; Li, YN.Nitrogen deposition impacts on the amount and stability of soil organic matter in an alpine meadow ecosystem depend on the form and rate of applied nitrogen,EUROPEAN JOURNAL OF SOIL SCIENCE,2014,65(4):510
|
| 出版日期 | 2014-07-01 |
| 英文摘要 | The effects of atmospheric nitrogen (N) deposition on carbon (C) sequestration in terrestrial ecosystems are controversial. Therefore, it is important to evaluate accurately the effects of applied N levels and forms on the amount and stability of soil organic carbon (SOC) in terrestrial ecosystems. In this study, a multi-form, small-input N addition experiment was conducted at the Haibei Alpine Meadow Ecosystem Research Station from 2007 to 2011. Three N fertilizers, NH4Cl, (NH4)(2)SO4 and KNO3, were applied at four rates: 0, 10, 20 and 40 kg N ha(-1) year(-1). One hundred and eight soil samples were collected at 10-cm intervals to a depth of 30 cm in 2011. Contents and delta C-13 values of bulk SOC were measured, as well as three particle-size fractions: macroparticulate organic C (MacroPOC, > 250 mu m), microparticulate organic C (MicroPOC, 53-250 mu m) and mineral-associated organic C (MAOC, < 53 mu m). The results show that 5 years of N addition changed SOC contents, delta C-13 values of the bulk soils and various particle-size fractions in the surface 10-cm layer, and that they were dependent on the amounts and forms of N application. Ammonium-N addition had more significant effects on SOC content than nitrate-N addition. For the entire soil profile, small additions of N increased SOC stock by 4.5% (0.43 kg C m(-2)), while medium and large inputs of N decreased SOC stock by 5.4% (0.52 kg C m(-2)) and 8.8% (0.85 kg C m(-2)), respectively. The critical load of N deposition appears to be about 20 kg N ha(-1) year(-1). The newly formed C in the small-input N treatment remained mostly in the > 250 mu m soil MacroPOC, and the C lost in the medium or large N treatments was from the > 53 mu m POC fraction. Five years of ammonium-N addition increased significantly the surface soil POC:MAOC ratio and increased the instability of soil organic matter (SOM). These results suggest that exogenous N input within the critical load level will benefit C sequestration in the alpine meadow soils on the Qinghai-Tibetan Plateau over the short term.; The effects of atmospheric nitrogen (N) deposition on carbon (C) sequestration in terrestrial ecosystems are controversial. Therefore, it is important to evaluate accurately the effects of applied N levels and forms on the amount and stability of soil organic carbon (SOC) in terrestrial ecosystems. In this study, a multi-form, small-input N addition experiment was conducted at the Haibei Alpine Meadow Ecosystem Research Station from 2007 to 2011. Three N fertilizers, NH4Cl, (NH4)(2)SO4 and KNO3, were applied at four rates: 0, 10, 20 and 40 kg N ha(-1) year(-1). One hundred and eight soil samples were collected at 10-cm intervals to a depth of 30 cm in 2011. Contents and delta C-13 values of bulk SOC were measured, as well as three particle-size fractions: macroparticulate organic C (MacroPOC, > 250 mu m), microparticulate organic C (MicroPOC, 53-250 mu m) and mineral-associated organic C (MAOC, < 53 mu m). The results show that 5 years of N addition changed SOC contents, delta C-13 values of the bulk soils and various particle-size fractions in the surface 10-cm layer, and that they were dependent on the amounts and forms of N application. Ammonium-N addition had more significant effects on SOC content than nitrate-N addition. For the entire soil profile, small additions of N increased SOC stock by 4.5% (0.43 kg C m(-2)), while medium and large inputs of N decreased SOC stock by 5.4% (0.52 kg C m(-2)) and 8.8% (0.85 kg C m(-2)), respectively. The critical load of N deposition appears to be about 20 kg N ha(-1) year(-1). The newly formed C in the small-input N treatment remained mostly in the > 250 mu m soil MacroPOC, and the C lost in the medium or large N treatments was from the > 53 mu m POC fraction. Five years of ammonium-N addition increased significantly the surface soil POC:MAOC ratio and increased the instability of soil organic matter (SOM). These results suggest that exogenous N input within the critical load level will benefit C sequestration in the alpine meadow soils on the Qinghai-Tibetan Plateau over the short term. |
| 源URL | [http://ir.nwipb.ac.cn/handle/363003/4214]  |
| 专题 | 西北高原生物研究所_中国科学院西北高原生物研究所 |
| 推荐引用方式 GB/T 7714 | Fang, H. J.,Cheng, S. L.,Yu, G. R.,et al. Nitrogen deposition impacts on the amount and stability of soil organic matter in an alpine meadow ecosystem depend on the form and rate of applied nitrogen[J]. EUROPEAN JOURNAL OF SOIL SCIENCE, Fang, HJ; Cheng, SL; Yu, GR; Yang, XM; Xu, MJ; Wang, YS; Li, LS; Dang, XS; Wang, L; Li, YN.Nitrogen deposition impacts on the amount and stability of soil organic matter in an alpine meadow ecosystem depend on the form and rate of applied nitrogen,EUROPEAN JOURNAL OF SOIL SCIENCE,2014,65(4):510,2014. |
| APA | Fang, H. J..,Cheng, S. L..,Yu, G. R..,Yang, X. M..,Xu, M. J..,...&Li, Y. N..(2014).Nitrogen deposition impacts on the amount and stability of soil organic matter in an alpine meadow ecosystem depend on the form and rate of applied nitrogen.EUROPEAN JOURNAL OF SOIL SCIENCE. |
| MLA | Fang, H. J.,et al."Nitrogen deposition impacts on the amount and stability of soil organic matter in an alpine meadow ecosystem depend on the form and rate of applied nitrogen".EUROPEAN JOURNAL OF SOIL SCIENCE (2014). |
入库方式： OAI收割
来源：西北高原生物研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。