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陕北半干旱黄土区陡坡微地形分布规律
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摘要
微地形导致陕北半干旱黄土区坡面水分的异质性,因此按照微地形进行植被配置是解决该地区植被恢复困难问题的重要理论。本文选取陕西省吴起县合沟流域为研究对象,基于三维影像扫描全站仪、GIS、统计学等方法,研究黄土丘陵沟壑区陡坡微地形分布规律。研究结果表明:以卷尺测量值为参照,三维影像扫描全站仪测量的浅沟长度和陡坎宽度误差均在5%左右,能够满足本文对微地形研究的需要;五种微地形占坡面面积比例平均值从大大小依次为切沟8.44%、缓台6.66%、浅沟5.00%、陡坎1.53%、塌陷1.52%;陡坡坡面陡坎与塌陷占坡面面积比例上限介于2%-5%之间、浅沟与切沟占坡面面积比例上限介于5%-10%之间、缓台占坡面面积比例上限介于15%-20%之间;塌陷、浅沟和切沟占坡面面积比例整体表现为阳坡和半阳坡大于半阴坡和阴坡,陡坎占坡面面积比例表现为阴坡和半阳坡大于半阴坡和阳坡,而相反,缓台表现为半阴坡和阳坡大于阴坡和半阳坡;陡坎、浅沟和切沟占坡面面积比例随着坡度的增大而减小,塌陷占坡面面积比例随着坡度的增大而增大;田坎与沟缘线对塌陷、陡坎和缓台等三种微地形的面积、长度、汇流面积及上坡坡长等地形参数有不同的影响;按照微地形进行植被配置后能有较大比例的乔灌植被。
The microrelief lead to soil moisture heterogeneity on slop,therefore,According to microrelief in configuring vegetation is an important theory to solve the difficult restoration of vegetation on steep slop in semiarid loess area in north Shaanxi Province.Choosing He Vally in Wuqi County,Shanxi Province as research object,based on3-d laser scanner, GIS and significant to research microrelief distribution in steep slope in loess hilly and gully region.The results showed that comaring with tape measure results, the error is about5%of shallow gully length and scarp width measured by3-d laser scannerwhi,ch is satisfied for researching microrelief;The area percentage of differerent microrelief,from big to small,are gully (8.44%), platform(6.66%), shallow gully (5.00%),scarp(1.53%) and collapse(1.52%).The area percentage upper of scarp and collapse is between2%-5%,gully and shallow gully is between10%-15%,platform is between15%-20%; the area percentage of collapse,gully and shallow gully shown as sunny slope and half-sunny slope are higher than half-shaded slope and shaded slope,however,it shows an opposite result of scarp area percentage. The area percentage of scarp,gully and shallow gully increases with slope gradient,and The area percentage of collapse decrease with slope gradient. The ridge and valley shoulder line have different effection on the terrain parameter,such as area,length,slope gradient and confluence area of collapse,scarp and platform; in addition, According to microrelief in configuring vegetation, arbor and shrub vegetation can take a big proportion.
引文
[1]陈永宗.黄土陷穴的成因及危害[J].地理学资料,1958,23(3):32-39.
    [2]陈永宗.黄土高原现代侵蚀与治理[M].北京,科学出版社:1988
    [3]程宏,王升堂,伍永秋,张春来.坑状浅沟侵蚀研究[J].水土保持学报,2006,20(2):39-41,58
    [4]邓慧平,李秀彬.地形指数的物理意义分析[J].地理科学进展.2002,21(2):103-110
    [5]唐克丽,郑世清,席道勤,孙清芳,刘斌武.杏子河流域坡耕地的水土流失及其防治[J].水土保持通报,1983,3(5):43-48
    [6]董华英,董婕.黄土高原植被建设中的问题与对策探讨[J].国土与自然资源研究,2007,1:64-65
    [7]窦家国,王文龙,郭军权.黄土丘陵沟壑区浅沟水流水动力学参数实验研究[J].中国水土保持科学,2008,6(1):93-100.
    [8]胡刚,伍永秋,刘宝元,郑秋红,张永光,刘洪鹄.东北漫岗黑土区切沟侵蚀发育特征[J].地理学报,2007,62(11):1165-1173
    [9]胡刚,伍永秋.发生沟蚀(切沟)的地貌临界研究综述[J].山地学报,2005,23(5):565-570
    [10]胡世雄,靳长兴.坡面土壤侵蚀临界坡度问题的理论与试验研究[J].地理学报,1999,54(4):348-356
    [11]霍云云,吴淑芳,冯浩,原立峰.基于三维激光扫描全站仪的坡面细沟侵蚀动态过程研究[J].中国水土保持科学,2011,9(2):32-37
    [12]何福红,黄明斌,党廷辉.黄土高原沟壑区小流域土壤水分空间分布特征[J].水土保持通报,2002,22(4):6-9
    [13]姜永清,王占礼,胡光荣,郝小品.瓦背状浅沟分布特征分析[J].水土保持研究,1999,6(2):182-184
    [14]景可.黄土高原沟谷侵蚀研究[J].地理科学,1986,6(4):340-347
    [15]景可,郑粉莉.黄土高原植被建设的经验教训与前景分析[J].水土保持研究,2004,11(4):25-27,178
    [16]刘文兆.半干旱黄土丘陵区小流域横断面土壤水分生态特征[J].干旱地区农业研究,2003,21(4):95-100.
    [17]梁守伦,郭翠萍,张炜.晋西黄土丘陵区立地类型划分的研究(Ⅱ):立地类型划分的研究[J].山西林业科技,2004,1(3):6-10
    [18]靳长兴.论坡面侵蚀的临界坡度[J].地理学报,1995,50(3):234-239
    [19]吕殿青,潘云.六道沟流域不同坡位不同土地利用方式下的土壤持水特征研究[J].中国农学通报,2008,24(8):279-282
    [20]路保昌,薛智德,朱清科,李会科.干旱阳坡半阳坡微地形土壤水分分布研究[J].水土保持通报,2009,29(1):62-65
    [21]李斌兵,郑粉莉,张鹏.黄土高原丘陵沟壑区小流域浅沟和切沟侵蚀区的界定[J].水土保持通报,2008,28(5):16-20
    [22]李斌兵,郑粉莉,龙栋材,江忠善.基于GIS纸坊沟小流域土壤侵蚀强度空间分布[J].地理科学,2009,29(1):105-110
    [23]李鹏.黄土区草地植被水土保持作用机理试验研究[D].陕西杨陵:西北农林科技大学,2003
    [24]李安怡,吴秀芹,朱清科.陕北黄土区浅沟分布特征及其与立地类型的关系[J].西北农林科技大学学报(自然科学版),2010,38(4):79-85
    [25]Majid Soufi澳大利亚一个林地环境下的切沟发展过程和侵蚀趋势研究[J].中国水土保持,2002,(7):26-29
    [26]马祥华,白文娟、焦菊英、焦峰.黄土丘陵沟壑区退耕地植被恢复中的土壤水分变化研究[J].水土保持通报,2004,24(5):19-23
    [27]马娟霞,肖玲,关帅朋等.黄土高原刺槐林地土壤水分与立地因子关系研究[J].土壤通报,2010,41(6):1311-1315
    [28]秦伟,朱清科,赵磊磊,等.基于RS和GIS的黄土丘陵沟壑区浅沟侵蚀地形特征研究[J].农业工程学报,2010,26(6):58-64
    [29]全国土壤普查办公室.中国土壤[M].北京:中国农业出版社,1998
    [30]邱扬,傅伯杰,王军,陈利顶.黄土丘陵小流域土壤水分的空间异质性及其影响因子[J].应用生态学报,2001,12(5):715-720
    [31]孙中峰,张学培.晋西黄土区坡面尺度土壤水分分布规律研究[J].水土保持通报,2006,26(2):27-30.
    [32]卫伟,陈利顶,傅伯杰,巩杰.半干旱黄土丘陵沟壑区降水特征值和下垫面因子影响下的水土流失规律[J].生态学报,2006,26(11):847-853
    [33]王晶,朱清科,赵荟,云雷,刘中奇,邝高明,谢静.陕北黄土区阳坡微地形土壤水分特征研究[J].水土保持通报,2011,8(4):16-21
    [34]王斌科.引起洞穴侵蚀的主要因素的探索[J].水土保持学报,1989,3(3):84-90.
    [35]伍永秋,刘宝元.切沟、切沟侵蚀与预报[J].应用基础与工程科学学报,2000,8(2):134-142
    [36]武敏,郑粉莉,黄斌.黄土坡面汇流汇沙对浅沟侵蚀影响的试验研究[J].水土保持研究,2004,11(4):70-76,90
    [37]徐海燕,赵文武,刘国彬,朱恒峰,朱婧,解纯营.黄土丘陵沟壑区坡面尺度土地利用格局变化对径流的影响[J].水土保持通报,2008,28(6):49-52,72
    [38]于章涛,伍永秋.黑土地切沟侵蚀的成因与危害[J].北京师范大学学报(自然科学版),2003,39(5):701-705
    [39]杨华.山西吉县黄土区切沟分类的研究[J].北京林业大学学报,2001,23(1):38-43
    [40]赵鹏祥,徐国策,王鸿哲,等.基于GIS的陕北农牧交错带立地类型划分研究[J].西北农林科技大学学报:自然科学版,2009,37(10):76-82
    [41]赵荟,朱清科,秦伟,刘中奇,王晶,邝高明.黄土高原干旱阳坡微地形土壤水分特征研究[J].水土保持通报,2010,30(3):64-68
    [42]张宏芝.陕北黄土坡面微地形土壤质量研究[D].北京:北京林业大学,2011
    [43]张科利.陕北黄土丘陵沟壑区坡耕地浅沟及其防治途径[D].陕西杨陵:中国科学院水利部水土保持研究所,1988
    [44]张科利,唐克丽.浅沟发育与陡坡开垦历史的研究[J].水土保持学报,1992,6(2):59-62,67
    [45]张姣,郑粉莉,温磊磊,俞方圆,安娟,李桂芳.利用三维激光扫描技术动态监测沟蚀发育过程的方法研究[J].水土保持通报,2011,31(6):89-94
    [46]张鹏,郑粉莉,王彬,陈吉强,丁晓斌.高精度GPS,三维激光扫描和测针板三种测量技术监测沟蚀过程的对比研究[J].水土保持通报,2008,28(5):11-15,20
    [47]张新和,郑粉莉,李靖.切沟侵蚀研究现状与存在问题分析[J].水土保持研究,2007,14(4):31-32,36
    [48]郑宝明,田承宏,王煜.黄土丘陵沟壑区第一副区小流域坝系建设理论与实践[M].郑州:黄河出版社:2004
    [49]郑粉莉,武敏,张玉斌,丁晋利.黄土陡坡裸露坡耕地浅沟发育过程研究[J].地理科学,2006,26(4):438-442.
    [50]郑粉莉,高学田.坡面土壤侵蚀过程研究进展[J].地理科学,2003,23(2):230-235
    [51]郑粉莉,唐克丽,周佩华.黄土高原坡耕地的细沟侵蚀及其防治途径[D].陕西杨陵:中国科学院西北水土保持研究所,1983
    [52]郑粉莉,高学田.黄土坡面土壤侵蚀过程与模拟[M].西安:陕西人民出版社,2000
    [53]郑良勇.黄土地区陡坡水蚀动力过程试验研究[D].陕西杨陵:西北农林科技大学,2003
    [54]周佩华,徐国礼,鲁翠瑚,刘建凯.黄土高原的侵蚀沟及其摄影测量方法[J].水土保持通报,1984,4(5):38-42
    [55]朱显谟.黄土区的洞穴侵蚀[J].黄河建设,1958,22(3):118-123.
    [56]曾伯庆.晋西黄土丘度沟壑区水土流失规律及治理效益[J].人民黄河,1980,(2):20-24
    [57]Bocco G.Gully erosion:processes and models[J].Progress in Physical Geography,1991, 15(4):392-406
    [58]Brice,J.B.Erosion and deposition in the loess mantled Great Plains[M].Medicine Creek drainage basin,Nebraska.U.S.Geol.Survey Prof.Paper,1966,352:235-339
    [59]Begin,z.B.and Schumm,S.A.Instability of alluvial valley floors:a method for its assessment[J].Trans.Am.Soc.Agric.Eng,1979,22:347-350
    [60]Casali J Bennett,S Robinson K.Processesof ephemeral gully erosion[J].International Journal of Sediment Research,2000,15(1):31-41
    [61]Grissinger E H,Murphey C E.Ephemeral gully erosion in the loess uplands,Goodwin Creek watershed.Northern Mississippi[M].Beijing:USA.Final Proc.Int.Conf.River Sedimentation. 1989,51-58
    [62]Horton,R.E.Erosional development of streams and theirdrainage basins;hydrophysical approach to quantitative morphology[J].Geol.Soc.Am.Bull.1945,56:275-370
    [63]Hawley M.E, Jackson T.J, Mccuen R.H.Surface soil moisture variation on small agricultural watersheds[J].Journal of Hydrology,1983,62:179-200.
    [64]J.Casah,J.Loizu,M.A.Campo, L.M. De Santisteban, J. A lvarez-Mozos. Accuracy of methods for field assessment of rill and ephemeral gully erosion[J]. Catena,2006,67:128-138
    [65]Martin Z,Penela A J.Pipe and gully systems development in the Almanzora Basin(Southeast Spain)[J].Geomorphy N F,1994,38(2):207-222
    [66]Marzolff a, J. Poesen. The potential of 3D gully monitoring with GIS using high-resolution aerial photography and a digital photogrammetry system[J]. Geomorphology,2009,111:48-60
    [67]Nagamatsu D andMirura O. Soil disturbance regime in relation to micro-scale landforms and its effects on vegetation structure in a hilly area in Japan[J]. Plant Ecology,1997,133: 191-200.
    [68]Oliveira M A T.Slope geometry and gully erosion development:Bannanal,A SO Paulo,Brazil[J],Z Geomorph N F,1990,34(4):423-434
    [69]Piest R F,Spomer R C.Sheet and gully erosion in the Missouri valley loessial region [J].Trans.ASAE,1968,11 (6):850-853
    [70]Posen J,Nachtergael J,Verstraeten G,et.al.Gully erosion and environmental change importance and research needs[J].Catena,2003,50,91-133
    [71]Patton,P.C.Gully erosion in the semi-arid West.M.Sc.Thesis[J].Fort Collins,Colorado State University,1973,129
    [72]Piest R F,Bradford J M,Spomer R G.Mechanimism of erosion and sediment movement from gullies[M].USDA:Present and Prospective Technology for Predicting Sediment Yields and Sources,ARS-S-40.ARS-USDA,Washington DC,1975.162-176
    [73]Sidorchuk A.Dynamic and static models of gully erosion[J].Catena,1999,37(3-4):401-414
    [74]Schurnm,S.A.Evolution of drainage systems and slopes in bad lands at Perth Amboy[J].NewJersey Bulletin Geological Society America,1956,67:597-646
    [75]Zheng Fenli,Huang Chi-hua.Gully erosion[A].In:Lal Rattan edited.Encyclopedia of soil science [M].New York:M arcel Dekker Inc,2002:630-634

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