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黄土高原丘陵区冰草和柳枝稷土壤细沟可蚀性季节动态

郁耀闯, 王长燕

郁耀闯, 王长燕. 黄土高原丘陵区冰草和柳枝稷土壤细沟可蚀性季节动态[J]. 草业科学, 2017, 11(5): 950-957. DOI: 10.11829/j.issn.1001-0629.2016-0346
引用本文: 郁耀闯, 王长燕. 黄土高原丘陵区冰草和柳枝稷土壤细沟可蚀性季节动态[J]. 草业科学, 2017, 11(5): 950-957. DOI: 10.11829/j.issn.1001-0629.2016-0346
Yao-chuang Yu, Chang-yan Wang. Seasonal dynamics of soil rill erodibility under wheatgrass and switchgrass vegetation in the hilly-gully region of Loess Plateau[J]. Pratacultural Science, 2017, 11(5): 950-957. DOI: 10.11829/j.issn.1001-0629.2016-0346
Citation: Yao-chuang Yu, Chang-yan Wang. Seasonal dynamics of soil rill erodibility under wheatgrass and switchgrass vegetation in the hilly-gully region of Loess Plateau[J]. Pratacultural Science, 2017, 11(5): 950-957. DOI: 10.11829/j.issn.1001-0629.2016-0346

黄土高原丘陵区冰草和柳枝稷土壤细沟可蚀性季节动态

基金项目: 

国家自然科学基金项目(41371497、41171423、41601016)

陕西省教育厅重点实验室项目(2010JS072、2009JS071)

宝鸡文理学院重点科研项目(ZK2017039、ZK2017040)

摘要: 为了评价黄土高原丘陵区退耕还草水土保持效应,本研究以黄土丘陵区冰草(Agropyron cristatum)和柳枝稷(Panicum virgatum)为研究对象,在不同坡度(S=17.36%~42.26%)和流量(Q=1.0~2.5 L·s-1)条件下,采用变坡试验水槽测定土壤的分离能力,利用线性回归方法,结合土壤侵蚀过程,运用WEPP模型推求土壤细沟可蚀性(Kr),分析了冰草和柳枝稷生育期内土壤Kr的季节变化规律。结果表明,黄土丘陵区冰草生育期内土壤Kr具有显著的季节变化(P<0.05),总体呈下降趋势;柳枝稷生育期内土壤Kr无显著季节变化(P>0.05)。冰草土壤Kr表现为下降的季节变化,变化范围为0.002 1~0.022 4 s·m-1;柳枝稷土壤Kr表现为先升高后降低的季节变化,变化范围为0.003 2~0.021 9 s·m-1。土壤黏结力、水稳性团聚体和根重密度是影响冰草和柳枝稷生育期内土壤Kr季节变化的主要因素。土壤细沟可蚀性与土壤黏结力、水稳性团聚体及根重密度间呈显著负相关关系。此外,用土壤黏结力和根重密度能够较好地模拟黄土丘陵区冰草和柳枝稷生育期内土壤细沟可蚀性的季节变化。冰草和柳枝稷土壤细沟可蚀性季节变化主要由根系生长和土壤黏结力变化所致。土壤细沟可蚀性与土壤黏结力、水稳性团聚体和根重密度间呈显著负相关关系。用土壤黏结力和根重密度等参数能够较好地模拟冰草和柳枝稷土壤细沟可蚀性的季节变化规律。

 

English

  • [1]

    Yang Y S.A study on the erodibility of parplish soil under different land utilization forms.Journal of Soil and Sater Conservation,1992,6(3):52-58.(in Chinese)

    [1]

    Zheng F L.Effect of vegetation changes on soil erosion on the Loess Plateau.Pedosphere,2006,16(4):420-427.

    [2]

    Fu B J,Liu Y,Lu Y H,He C S,Zeng Y,Wu B F.Assessing the soil erosion control service of ecosystems change in the Loess Plateau of China.Ecological Complexity,2011,8(4):284-293.

    [2]

    Deng L J,Hou D B,Wang C Q,Zhang S R,Xia J G.Study on soil erodibility of natural soil and dry farmland soil in Sichuan.Soil and Water Conservation in China,2003(7):23-25.(in Chinese)

    [3]

    Liang Y,Liu X C,Cao L X,Zheng F L,Zhang P C,Shi M C,Cao Q Y,Yuan J Q.The calculation and macroscopic distribution of soil erodibility K value in China#x02019;s water erosion area.Soil and Water Conservation in China,2013(10):35-40.(in Chinese)

    [3]

    Zhang X C,Liu W Z.Simulating potential response of hydrology,soil erosion,and crop productivity to climate change in Changwu tablel and region on the Loess Plateau of China.Agricultural #x00026; Forest Meteorology,2005,131(3-4):127-142.

    [4]

    Zhang K L,Cai Y M,Liu B Y,Peng W Y.Fluctuation of soil erodibility due to rainfall intensity.Acta Geographica Sinica,2001,56(6):673-681.(in Chinese)

    [4]

    Chen Y P,Wang K B,Lin Y S,Shi W Y,Song Y,He X H.Balancing green and grain trade.Nature Geoscience,2015,8(10):739-741.

    [5]

    Angers D A,Caron J.Plant-induced changes in soil structure:Processes and feedbacks.Biogeochemistry,1998,42(1-2):55-72.

    [5]

    Wang B.Dynamic mechanism of soil erodibility and soil erodibility calculation model.PhD Thesis.Yangling:Northwest Agriculture #x00026; Forest University,2013.(in Chinese)

    [6]

    Liu B Y,Shi P J.Water erosion prediction project (WEPP) model for watershed scale.Bulletin of Soil and Water Conservation,1998,18(5):6-12.(in Chinese)

    [6]

    Li Y Y,Shao M A.Change of soil physical properties under long-term natural vegetation restoration in the Loess Plateau of China.Journal of Arid Environments,2006,64(1):77-96.

    [7]

    Jiao F,Wen Z M,An S S.Changes in soil properties across a chronosequence of vegetation restoration on the Loess Plateau of China.Catena,2011,86(2):110-116.

    [7]

    Wu C G,Zeng Y,Zhou Z X,Wang P C,Xiao W F,Luo C.Soil erodibility K value in three gorges reservoir area.Science of Soil and Water Conservation,2010,8(3):8-12.(in Chinese)

    [8]

    Hirschi M C,Barfield B J.KYERMO#x02014;#x02014;A physically based research erosion model.Part #x02160;.Model development.Transactions of the American Society of Agricultural Biological Engineers,1988,31(3):804-813.

    [8]

    Zhou N,Li C,Ju C Y,Ma Y H.Analysis of characteristics of soil erodibility K value in Heilongjiang Province.Transactions of the Chinese Society of Agricultural Engineering,2015,31(10):182-189.(in Chinese)

    [9]

    Wang L N,Li W L,Wang S F,Chen D,Xu J.Variation in soil erosion based on USLE model and remote sensing technology during 2000-2010 in Gansu Province.Pratacultural Science,2016,33(2):176-183.(in Chinese)

    [9]

    Nearing M A,Foster G R,Lane L J,Finkner S C.A process-based soil erosion model for USDA-water erosion prediction technology.Transactions of the American Society of Agricultural Engineers,1989,32(5):1587-1593.

    [10]

    Zhang X Y,Zhou Z C.Research progress on mechanism of grassland vegetation regulating soil erosion in Loess Plateau.Pratacultural Science,2015,32(1):64-70.(in Chinese)

    [10]

    Flanagan D C,Nearing M A.Water erosion prediction project (WEEP) model.Landscape Erossion and Evolution Modeling,2001,53(5):1399-1411.

    [11]

    Li Y,Wu Q X,Zhu X M,Tian J Y.Studies on the intensification of soil anti-scourability by plant roots in the Loess Plateau #x02160;.The increasing effect of soil anti-scourability by the roots of Chinese Pine.Journal of Soil and Water Conservation,1990,4(1):1-5.(in Chinese)

    [11]

    Knapen A,Poesen J,Govers G,Gyssels G,Nachtergaele J.Resistance of soils to concentrated flow erosion:a review.Earth Science Reviews,2007,80(1):75-109.

    [12] 杨玉盛.不同利用方式下紫色土可蚀性的研究.水土保持学报,1992,6(3):52-58.
    [13] 邓良基,侯大斌,王昌全,张世熔,夏建国.四川自然土壤和旱耕地土壤可蚀性特征研究.中国水土保持,2003(7):23-25.
    [14] 梁音,刘宪春,曹龙熹,郑粉莉,张平仓,史明昌,曹全意,袁久芹.中国水蚀区土壤可蚀性 K值计算与宏观分布.中国水土保持,2013(10):35-40.
    [15] 张科利,蔡永明,刘宝元,彭文英.土壤可蚀性动态变化规律研究.地理学报,2001,56(6):673-681.
    [16] 王彬.土壤可蚀性动态变化机制与土壤可蚀性估算模型.杨凌:西北农林科技大学博士学位论文,2013.
    [17] 刘宝元,史培军.WEPP水蚀预报流域模型.水土保持通报,1998,18(5):6-12.
    [18] 吴昌广,曾毅,周志翔,王鹏程,肖文发,罗翀.三峡库区土壤可蚀性K值研究.中国水土保持科学,2010,8(3):8-12.
    [19] 周宁,李超,琚存勇,马亚怀.黑龙江省土壤可蚀性K值特征分析.农业工程学报,2015,31(10):182-189.
    [20] 王莉娜,李文龙,王素芳,陈迪,许静.基于遥感和USLE模型的2000-2010年甘肃省土壤侵蚀变化评价.草业科学,2016,33(2):176-183.
    [21]

    Zhang G H,Tang K M,Zhang X C.Temporal variation in soil detachment under different land uses in the Loess Plateau of China.Earth Surface Processes and Landforms,2009,34(9):1302-1309.

    [22]

    Nearing M A,Simanton J R,Norton L D,Bulygin S J,Stone J.Soil erosion by surface water flow on a stony,semiarid hillslope.Earth Surface Processes and Landforms,1999,24(8):677-686.

    [23]

    Knapen A,Poesen J,De Baets S.Seasonal variations in soil erosion resistance during concentrated flow for a loess-derived soil under two contraxting tillage practices.Soil and Tillage Research,2007,94(2):425-440.

    [24]

    Yu Y C,Zhang G H,Geng R,Li Z W.Temporal variation in soil rill erodibility to concentrated flow detachment under four typical croplands in the Loess Plateau of China.Journal of Soil and Water Conservation,2014,69(4):352-363.

    [25]

    Norris J E.Root reinforcement by hawthorn and oak roots on a highway cut-slope in southern England.Plant #x00026; Soil,2005,278(1-2):43-53.

    [26]

    Baets S de,Poesen J,Gyssels G,Knapen A.Effects of grass on the erodibility of topsoil during concentrated flow.Geomorphology,2006,76(1-2):54-67.

    [27]

    Tengbeh G T.The effect of grass roots on shear strength variations with moisture content.Soil Technology,1993,6(3):287-295.

    [28]

    Wang B,Zhang G H,Zhang X C,Li Z W,Su Z L,Yi T,Shi Y Y.Effects of near soil surface characteristics on soil detachment by overland flow in a natural succession grassland.Soil Science Society of America Journal,2014,78(59):589-597.

    [29]

    Coote D R,Malcolmmcgovern M C A,Wall G J,Dickinson W T,Rudra R P.Seasonal variations of erodibility indices based on shear strength and aggregate stability in some Ontario soils.Canadian Journal of Soil Science,1988,68(2):405-416.

    [30] 张晓艳,周正朝.黄土高原地区草地植被调控土壤水蚀机理的研究进展.草业科学,2015,32(1):64-70.
    [31] 李勇,吴钦孝,朱显谟,田积莹.黄土高原植物根系提高土壤抗冲性能的研究.#x02160;.油松人工林根系对土壤抗冲性的增强效应.水土保持学报,1990,4(1):1-5.
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  • 收稿日期:  2016-06-26
  • 修回日期:  2017-01-02
  • 发布日期:  2017-05-19

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