Organic carbon losses by eroded sediments from sloping vegetable fields in South China
文献类型：期刊论文
| 作者 | QIAN Jing; ZHANG Li-ping; WANG Wen-yan; LIU Qiao |
| 刊名 | Journal of Mountain Science
 |
| 出版日期 | 2017-03 |
| 卷号 | 14期号:3页码:539-548 |
| 关键词 | Fertilizer Treatment Particle-size Distribution Vegetation Cover Ratio Sediment Yields Slope Length Soil Organic Carbon Surface Runoff |
| ISSN号 | 1672-6316 |
| DOI | 10.1007/s11629-016-3845-2 |
| 通讯作者 | ZHANG Li-ping |
| 文献子类 | 期刊论文 |
| 英文摘要 | Soil Organic Carbon (SOC) is the most important component of soil. Though small, it determines soil fertility and prevents soil losses. In this study, we examined relationships between the Particle–Size Distribution(PSD) of the eroded sediment and SOC loss, and evaluated the effects of plant coverage ratios (0%, 15%, 30%, 45%, 60% and 90%), slope lengths (2 m, 4 m), fertilizer treatments (unfertilized control (CK), compound N–P–K fertilizer (CF), and organic fertilizer (OF)) on SOC loss and the SOC enrichment ratio (ERSOC) in the eroded sediments. The experimental results showed that longer slope length and lower surface cover ratios produced larger surface runoff and the eroded sediments, resulting in larger SOC losses. The average SOC loss was greatest in the OF treatment and SOC loss was mainly associated with the eroded sediment. Surface runoff, which causes soil erosion, is a selective transportation process, hence there were more clay-sized particles (<2 μm) and silt-sized particles (2-50 μm) in the eroded sediments than in the original soils. SOC was enriched in the eroded sediments relative to in the original soil when ERSOC > 1. ERSOC was positively correlated with ERclay (<2 μm) (R2= 0.68) and ERfine silt (2–20 μm) (R2= 0.63), and from all the size particle categories of the original soil or the eroded sediments, more than 95% of SOC was concentrated in small-sized particles (<50 μm). The distribution of SOC in different-sized particles of the original soil and the eroded sediment is primarily associated with clay-sized particles and fine silt-sized particles, thus we conclude that as the eroded sediment particles became finer, more SOC was absorbed, resulting in more severe SOC loss. |
| 语种 | 英语 |
| 源URL | [http://ir.imde.ac.cn/handle/131551/18440]  |
| 专题 | Journal of Mountain Science _Journal of Mountain Science-2017_Vol14 No.3 |
| 推荐引用方式 GB/T 7714 | QIAN Jing,ZHANG Li-ping,WANG Wen-yan,et al. Organic carbon losses by eroded sediments from sloping vegetable fields in South China[J]. Journal of Mountain Science,2017,14(3):539-548. |
| APA | QIAN Jing,ZHANG Li-ping,WANG Wen-yan,&LIU Qiao.(2017).Organic carbon losses by eroded sediments from sloping vegetable fields in South China.Journal of Mountain Science,14(3),539-548. |
| MLA | QIAN Jing,et al."Organic carbon losses by eroded sediments from sloping vegetable fields in South China".Journal of Mountain Science 14.3(2017):539-548. |
入库方式： OAI收割
来源：成都山地灾害与环境研究所
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