Knowledge Resource Center for Ecological Environment in Arid Area
STUDY OF THE RELATIONSHIP BETWEEN DESERTIFICATION AND BLOWING SAND IN THE SANJIANGYUAN REGION IN QINGHAI-TIBETAN PLATEAU | |
Xu Mengzhen1,2; Li Yanfu3; Wang Zhaoyin1,2; Han Lujie1; Pan Baozhu4 | |
通讯作者 | Xu Mengzhen |
会议名称 | 36th IAHR World Congress |
会议日期 | JUN 28-JUL 03, 2015 |
会议地点 | Delft, NETHERLANDS |
英文摘要 | Desertification is defined as the phenomenon in which aeolian soil erosion happens, causing sand dunes to form and move, and deserts form due to climate change and human activities. Desertification in Qinghai-Tibetan Plateau where is most sensitive to climate changing, has become a focus of the world's ecological and environmental problems. Climate warming combining with anthropological activities has resulted in permafrost degradation, vegetation degeneration, sand dunes moving, and expanding of desertification in the plateau. In this study, field investigation and sampling were conducted in different active sand dunes, semi-fixed sand dunes, and fixed sand dunes for understanding the mechanism of desertification in Qinghai-Tibetan Plateau. Sediment composition of the active, semi-fixed, and fixed sand dunes were analyzed to identify the component (called "blowing sand") that plays the most important role in resulting in desertification. Desertification index (DDI), indicating the risk of desertification for an area, was defined as DDI=R(A)xa+R(SF)xs+R(F)xf+R(MS)xg, in which a, s, f, g indicates the different levels of desertification risk and are assigned as 1, 0.5, 0.25, and 0 for the active, semi-fixed, fixed sand dunes, and grasslands, respectively; R-A, R-SF, R-F, and R-MS are the proportions of the active, semi-fixed, fixed sand dunes, and grasslands in the sampled area. The relation between the percentage composition of blowing sand in each sediment sample and the desertification index of the sampled area was examined. It was found that blowing sand mainly composed of quartz mineral particles with grain sizes of 0.05 - 0.25 mm. The desertification would hardly occur when the percentage composition of blowing sand was lower than 50%, while the risk of desertification increased quadratically as the percentage composition of blowing sand increased when the percentage was higher than 60%. Therefore, the percentage composition of blowing sand is among the most important parameters resulting in desertification. Nevertheless, vegetation coverage is essential for controlling the proportions of the active, semi-fixed, and fixed sand dunes. Strategies helpful for reducing the proportion of blowing sand and promoting vegetation coverage are recommended for prevention of desertification in Qinghai-Tibetan Plateau. |
英文关键词 | Qinghai-Tibetan Plateau desertification index blowing sand grain size distribution mineral composition desertification control |
来源出版物 | PROCEEDINGS OF THE 36TH IAHR WORLD CONGRESS |
出版年 | 2015 |
页码 | 6108-6116 |
EISBN | 978-90-824846-0-1 |
出版者 | IAHR-INT ASSOC HYDRO-ENVIRONMENT ENGINEERING RESEARCH |
类型 | Proceedings Paper |
语种 | 英语 |
国家 | Peoples R China |
收录类别 | CPCI-S |
WOS记录号 | WOS:000398996206026 |
WOS类目 | Water Resources |
WOS研究方向 | Water Resources |
资源类型 | 会议论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/303742 |
作者单位 | 1.Tsinghua Univ, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China; 2.Tsinghua Univ, Sanjiangyuan Collaborat Innovat Ctr, Beijing 100084, Peoples R China; 3.Nanjing Hydraul Res Inst, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210029, Jiangsu, Peoples R China; 4.Changjiang River Sci Res Inst, Wuhan 430010, Peoples R China |
推荐引用方式 GB/T 7714 | Xu Mengzhen,Li Yanfu,Wang Zhaoyin,et al. STUDY OF THE RELATIONSHIP BETWEEN DESERTIFICATION AND BLOWING SAND IN THE SANJIANGYUAN REGION IN QINGHAI-TIBETAN PLATEAU[C]:IAHR-INT ASSOC HYDRO-ENVIRONMENT ENGINEERING RESEARCH,2015:6108-6116. |
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