Soil erosion rates and characteristics of typical alpine meadow using 137Cs technique in Qinghai-Tibet Plateau
Alpine meadow is the predominant ecosystem in Qinghai-Tibet Plateau. The firm turf of alpine meadow formed by sub-surface anfractuous roots can be effective in conserving water and soil. Alpine meadow is a primary contributor to the Chinese Water Tower. For quantitative assess anti-erosion ability o...
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Veröffentlicht in: | Chinese science bulletin 2011-06, Vol.56 (16), p.1708-1713 |
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description | Alpine meadow is the predominant ecosystem in Qinghai-Tibet Plateau. The firm turf of alpine meadow formed by sub-surface anfractuous roots can be effective in conserving water and soil. Alpine meadow is a primary contributor to the Chinese Water Tower. For quantitative assess anti-erosion ability of alpine meadow, this paper selected three typical meadow slopes with 〉60% vegetation coverage to evaluate soil erosion rates using 137Cs. The results showed that (1) soil erosion intensity of typical alpine meadow was slight to light. Erosion rates were 464 t km-2 a-1 in Malong Village, 415 t km-2 a-1 in Yeniugou Town and 875 t km-2 a-1 in Zhenqin Town respectively; (2) soil erosion rates were correlated negatively with vegetation coverage, and the relationship was clearer at the slope scale than plot scale; (3) the relationship between soil erosion and vegetation coverage showed that vegetation coverage was a predominant factor in retaining soil and water on slopes. With complete turf and high vegetation coverage, alpine meadow was of great significance for soil conservation and prevention of soil erosion. |
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The firm turf of alpine meadow formed by sub-surface anfractuous roots can be effective in conserving water and soil. Alpine meadow is a primary contributor to the Chinese Water Tower. For quantitative assess anti-erosion ability of alpine meadow, this paper selected three typical meadow slopes with 〉60% vegetation coverage to evaluate soil erosion rates using 137Cs. The results showed that (1) soil erosion intensity of typical alpine meadow was slight to light. Erosion rates were 464 t km-2 a-1 in Malong Village, 415 t km-2 a-1 in Yeniugou Town and 875 t km-2 a-1 in Zhenqin Town respectively; (2) soil erosion rates were correlated negatively with vegetation coverage, and the relationship was clearer at the slope scale than plot scale; (3) the relationship between soil erosion and vegetation coverage showed that vegetation coverage was a predominant factor in retaining soil and water on slopes. With complete turf and high vegetation coverage, alpine meadow was of great significance for soil conservation and prevention of soil erosion.</description><identifier>ISSN: 1001-6538</identifier><identifier>EISSN: 1861-9541</identifier><identifier>DOI: 10.1007/s11434-011-4477-0</identifier><language>eng</language><publisher>Heidelberg: Springer-Verlag</publisher><subject>137Cs ; alpine meadows ; Chemistry/Food Science ; correlation ; Earth Sciences ; Ecosystems ; Engineering ; Humanities and Social Sciences ; lawns and turf ; Life Sciences ; multidisciplinary ; Physics ; roots ; Science ; Science (multidisciplinary) ; Slopes ; Soil (material) ; Soil conservation ; Soil erosion ; soil water ; Towns ; Vegetation ; Villages ; 土壤侵蚀率 ; 土壤侵蚀速率 ; 技术 ; 植被覆盖度 ; 植被覆盖率 ; 青藏高原 ; 高寒草甸草地</subject><ispartof>Chinese science bulletin, 2011-06, Vol.56 (16), p.1708-1713</ispartof><rights>The Author(s) 2011</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2580-3fdf3db80dfd0eeebea24ae4a65e3a2863fc7ff9af50f82ac89053767dd59e1e3</citedby><cites>FETCH-LOGICAL-c2580-3fdf3db80dfd0eeebea24ae4a65e3a2863fc7ff9af50f82ac89053767dd59e1e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/86894X/86894X.jpg</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Shao, QuanQin</creatorcontrib><creatorcontrib>Xiao, Tong</creatorcontrib><creatorcontrib>Liu, JiYuan</creatorcontrib><creatorcontrib>Qi, YongQing</creatorcontrib><title>Soil erosion rates and characteristics of typical alpine meadow using 137Cs technique in Qinghai-Tibet Plateau</title><title>Chinese science bulletin</title><addtitle>Chin. Sci. Bull</addtitle><addtitle>Chinese Science Bulletin</addtitle><description>Alpine meadow is the predominant ecosystem in Qinghai-Tibet Plateau. The firm turf of alpine meadow formed by sub-surface anfractuous roots can be effective in conserving water and soil. Alpine meadow is a primary contributor to the Chinese Water Tower. For quantitative assess anti-erosion ability of alpine meadow, this paper selected three typical meadow slopes with 〉60% vegetation coverage to evaluate soil erosion rates using 137Cs. The results showed that (1) soil erosion intensity of typical alpine meadow was slight to light. Erosion rates were 464 t km-2 a-1 in Malong Village, 415 t km-2 a-1 in Yeniugou Town and 875 t km-2 a-1 in Zhenqin Town respectively; (2) soil erosion rates were correlated negatively with vegetation coverage, and the relationship was clearer at the slope scale than plot scale; (3) the relationship between soil erosion and vegetation coverage showed that vegetation coverage was a predominant factor in retaining soil and water on slopes. With complete turf and high vegetation coverage, alpine meadow was of great significance for soil conservation and prevention of soil erosion.</description><subject>137Cs</subject><subject>alpine meadows</subject><subject>Chemistry/Food Science</subject><subject>correlation</subject><subject>Earth Sciences</subject><subject>Ecosystems</subject><subject>Engineering</subject><subject>Humanities and Social Sciences</subject><subject>lawns and turf</subject><subject>Life Sciences</subject><subject>multidisciplinary</subject><subject>Physics</subject><subject>roots</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><subject>Slopes</subject><subject>Soil (material)</subject><subject>Soil conservation</subject><subject>Soil erosion</subject><subject>soil water</subject><subject>Towns</subject><subject>Vegetation</subject><subject>Villages</subject><subject>土壤侵蚀率</subject><subject>土壤侵蚀速率</subject><subject>技术</subject><subject>植被覆盖度</subject><subject>植被覆盖率</subject><subject>青藏高原</subject><subject>高寒草甸草地</subject><issn>1001-6538</issn><issn>1861-9541</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNp9kU-PFCEQxTtGE9fVD-BJPHlCKWga-mgm_ks2UbO7Z1JDFzNsemAWumP228umNx49UZD3Xh6_6rq3ID6CEOZTBehVzwUA73tjuHjWXYAdgI-6h-dtFgL4oJV92b2q9a7dFBh50aXrHGdGJdeYEyu4UGWYJuaPWNAvVGJdoq8sB7Y8nKPHmeF8jonYiXDKf9haYzowUGZX2UL-mOL9Siwm9ru9HzHym7inhf2aWzSur7sXAedKb57Oy-7265eb3Xd-9fPbj93nK-6ltoKrMAU17a2YwiSIaE8oe6QeB00KpR1U8CaEEYMWwUr0dhRamcFMkx4JSF12H7bcc8mtT13cKVZP84yJ8lrdCOPYq2FQTQmb0jcGtVBw5xJPWB4cCPeI1m1oXUPrHtE60Txy89SmTQcq7i6vJbUP_df0bjMFzA4PDay7vZYC-rYLYUGapnj_VOWY0-G-Jf_roqyQ2iit_gLwVpIK</recordid><startdate>20110601</startdate><enddate>20110601</enddate><creator>Shao, QuanQin</creator><creator>Xiao, Tong</creator><creator>Liu, JiYuan</creator><creator>Qi, YongQing</creator><general>Springer-Verlag</general><general>SP Science China Press</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>~WA</scope><scope>FBQ</scope><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SC</scope><scope>7SP</scope><scope>7SR</scope><scope>7TB</scope><scope>7U5</scope><scope>8BQ</scope><scope>8FD</scope><scope>FR3</scope><scope>JG9</scope><scope>JQ2</scope><scope>KR7</scope><scope>L7M</scope><scope>L~C</scope><scope>L~D</scope></search><sort><creationdate>20110601</creationdate><title>Soil erosion rates and characteristics of typical alpine meadow using 137Cs technique in Qinghai-Tibet Plateau</title><author>Shao, QuanQin ; 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Sci. Bull</stitle><addtitle>Chinese Science Bulletin</addtitle><date>2011-06-01</date><risdate>2011</risdate><volume>56</volume><issue>16</issue><spage>1708</spage><epage>1713</epage><pages>1708-1713</pages><issn>1001-6538</issn><eissn>1861-9541</eissn><abstract>Alpine meadow is the predominant ecosystem in Qinghai-Tibet Plateau. The firm turf of alpine meadow formed by sub-surface anfractuous roots can be effective in conserving water and soil. Alpine meadow is a primary contributor to the Chinese Water Tower. For quantitative assess anti-erosion ability of alpine meadow, this paper selected three typical meadow slopes with 〉60% vegetation coverage to evaluate soil erosion rates using 137Cs. The results showed that (1) soil erosion intensity of typical alpine meadow was slight to light. Erosion rates were 464 t km-2 a-1 in Malong Village, 415 t km-2 a-1 in Yeniugou Town and 875 t km-2 a-1 in Zhenqin Town respectively; (2) soil erosion rates were correlated negatively with vegetation coverage, and the relationship was clearer at the slope scale than plot scale; (3) the relationship between soil erosion and vegetation coverage showed that vegetation coverage was a predominant factor in retaining soil and water on slopes. With complete turf and high vegetation coverage, alpine meadow was of great significance for soil conservation and prevention of soil erosion.</abstract><cop>Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s11434-011-4477-0</doi><tpages>6</tpages><oa>free_for_read</oa></addata></record> |
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subjects | 137Cs alpine meadows Chemistry/Food Science correlation Earth Sciences Ecosystems Engineering Humanities and Social Sciences lawns and turf Life Sciences multidisciplinary Physics roots Science Science (multidisciplinary) Slopes Soil (material) Soil conservation Soil erosion soil water Towns Vegetation Villages 土壤侵蚀率 土壤侵蚀速率 技术 植被覆盖度 植被覆盖率 青藏高原 高寒草甸草地 |
title | Soil erosion rates and characteristics of typical alpine meadow using 137Cs technique in Qinghai-Tibet Plateau |
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