Climate Change Data Portal
| DOI | 10.1080/09064710903352589 |
| Effects of land use on temporal-spatial variability of soil water and soil-water conservation | |
| Zeng, Chen; Shao, Mingan; Wang, Quanjiu; Zhang, Jun | |
| 通讯作者 | Shao, MA (通讯作者) |
| 发表日期 | 2011 |
| ISSN | 0906-4710 |
| EISSN | 1651-1913 |
| 起始页码 | 1 |
| 结束页码 | 13 |
| 卷号 | 61期号:1 |
| 英文摘要 | The Loess Plateau of China suffers serious soil erosion primarily resulting from irrational land uses. Soil water plays a critical role influencing vegetation-restoration processes, but varies with temporal and spatial characteristics, of concern to many researchers. However, few studies consider the influence of deep soil water and varied weather patterns in a semi-arid region. Four vegetation types chosen for this study include artificial caragana shrubland, artificial alfalfa grassland, naturally restored vegetation land (Artemisia capillaries, Agropyron chistatum, Heteropapus altaicus Novop, Stipa bungeana, Stipa breviflora griseb and Lespedeza davurica), and bare land. Soil-water content at the top 400 cm depth was monitored continuously from 2004 to 2007 using a neutron probe. Water and wind soil erosion were investigated gravimetrically. Results showed that soil water varied greatly during May through October with different land-use types and annual precipitations. Soil water reached a lower level in both artificial vegetation lands in dry years but recharged with great variation in normal years. Soil water in two other lands tended to have similar changes with less variation as compared with the artificial vegetation lands. Soil water was intensively consumed with depth and continuously decreased in the deeper layers under the two artificial vegetations. The consumption in the artificial caragana shrubland was more intensive, while that in the artificial alfalfa grassland took place at greater depths. The naturally restored vegetation land had less soil-water consumption (close to the level in the bare land) as compared with the artificial vegetation lands. Soil-water content and its variability were increased along the slope with less variation over time. In general, both artificial vegetations effectively reduced the runoff and water-wind soil erosion in the third year after planting, while the naturally restored vegetation consistently showed weak conservation effects in the initial stage. |
| 关键词 | LOESS-PLATEAUMOISTURE PATTERNSRAINFALL INTENSITYHILLY AREASTABILITYEROSIONCHINACATCHMENTRUNOFFFIELD |
| 英文关键词 | Land use; runoff; soil water; temporal and spatial variability; The Loess Plateau of China; water-wind erosion |
| 语种 | 英语 |
| WOS研究方向 | Agriculture |
| WOS类目 | Agronomy ; Soil Science |
| WOS记录号 | WOS:000286923800001 |
| 来源期刊 | ACTA AGRICULTURAE SCANDINAVICA SECTION B-SOIL AND PLANT SCIENCE
 |
| 来源机构 | 中国科学院青藏高原研究所 |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/257954 |
| 推荐引用方式 GB/T 7714 | Zeng, Chen,Shao, Mingan,Wang, Quanjiu,et al. Effects of land use on temporal-spatial variability of soil water and soil-water conservation[J]. 中国科学院青藏高原研究所,2011,61(1). |
| APA | Zeng, Chen,Shao, Mingan,Wang, Quanjiu,&Zhang, Jun.(2011).Effects of land use on temporal-spatial variability of soil water and soil-water conservation.ACTA AGRICULTURAE SCANDINAVICA SECTION B-SOIL AND PLANT SCIENCE,61(1). |
| MLA | Zeng, Chen,et al."Effects of land use on temporal-spatial variability of soil water and soil-water conservation".ACTA AGRICULTURAE SCANDINAVICA SECTION B-SOIL AND PLANT SCIENCE 61.1(2011). |
| 条目包含的文件 | 条目无相关文件。 | |||||
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。
