Aeolian processes and their effect on sandy desertification of the Qinghai-Tibet Plateau: A wind tunnel experiment
文献类型：期刊论文
| 作者 | Wang, Xunming1,2; Lang, Lili1; Yan, Ping3; Wang, Guangtao2; Li, Hui2; Ma, Wenyong1; Hua, Ting2 |
| 刊名 | SOIL & TILLAGE RESEARCH
 |
| 出版日期 | 2016-05-01 |
| 卷号 | 158页码:67-75 |
| 关键词 | Sandy desertification Wind erosion Nutrient loss Human activity Wind tunnel simulation Qinghai-Tibet Plateau |
| ISSN号 | 0167-1987 |
| DOI | 10.1016/j.still.2015.12.004 |
| 通讯作者 | Wang, Xunming(xunming@lzb.ac.cn) |
| 英文摘要 | To determine the contribution of aeolian processes to sandy desertification, we applied different wind velocities to soils from the Qinghai-Tibet Plateau that were subjected to the human activities such as wholesale destruction of vegetation. We then employed field investigations, soil sampling in the field, wind tunnel experiments, particle size analyses, and nutrient analyses. After the ground surfaces were crushed to simulate land degradation, the aeolian transport in this region varied from 0.00 to 43.49 g m(-2) s(-1) and was dependent on the particle size composition, and variation in the intensity of aeolian processes. During the aeolian processes our wind tunnel results show differences between the nutrient contents of the transported materials and those of the surface soils, and the loss of total nitrogen (TN), total carbon (TC) and total phosphorus (TP) varied between 0.00 and 8.81, 0.10 and 122.27, 0.00 and 1.14 g m(-2), respectively. In addition, variations in wind velocities did not result in significant differences in the particle size fractions of the transported materials. On the Qinghai-Tibet Plateau, although an increase in human activity may trigger sandy desertification, the occurrence of sandy desertification was not significant in the early 21st century, and hence it is likely to be controlled by climate even though human impacts have undeniably exacerbated its effects. (C) 2015 Elsevier B.V. All rights reserved. |
| 收录类别 | SCI |
| WOS关键词 | LAND DEGRADATION ; SOURCE REGION ; SOIL PRODUCTIVITY ; EROSION PROCESSES ; BINDING-ENERGIES ; SEMIARID CHINA ; CLIMATE-CHANGE ; YELLOW-RIVER ; IN-SOURCE ; DESERT |
| WOS研究方向 | Agriculture |
| WOS类目 | Soil Science |
| 语种 | 英语 |
| WOS记录号 | WOS:000373244700008 |
| 出版者 | ELSEVIER SCIENCE BV |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2557264 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | Wang, Xunming |
| 作者单位 | 1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China 2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, Lanzhou 730000, Peoples R China 3.Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Xunming,Lang, Lili,Yan, Ping,et al. Aeolian processes and their effect on sandy desertification of the Qinghai-Tibet Plateau: A wind tunnel experiment[J]. SOIL & TILLAGE RESEARCH,2016,158:67-75. |
| APA | Wang, Xunming.,Lang, Lili.,Yan, Ping.,Wang, Guangtao.,Li, Hui.,...&Hua, Ting.(2016).Aeolian processes and their effect on sandy desertification of the Qinghai-Tibet Plateau: A wind tunnel experiment.SOIL & TILLAGE RESEARCH,158,67-75. |
| MLA | Wang, Xunming,et al."Aeolian processes and their effect on sandy desertification of the Qinghai-Tibet Plateau: A wind tunnel experiment".SOIL & TILLAGE RESEARCH 158(2016):67-75. |
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来源：寒区旱区环境与工程研究所
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