黄土丘陵沟壑区退耕坡地不同植物群落的土壤侵蚀特征

doi:10.16843/j.sswc.2017.03.014

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摘要黄土高原地区水土流失造成严重的农业和生态环境问题，而植被能从根本上控制黄土高原的水土流失。以安塞县典型退耕坡地不同植物群落为研究对象，采用侵蚀针法，结合2012-2015年降雨数据及不同植物群落特征的分析，研究不同植被恢复坡地的土壤侵蚀特征。结果表明：研究期间，不同年份植被群落土壤侵蚀强度为丰水年 > 平水年 > 枯水年。不同植被类型群落防治土壤侵蚀的能力不同，具体为自然恢复灌木群落 > 自然恢复草本群落 > 人工灌木群落 > 人工乔木群落。灰色关联度显示，降雨量与坡度是影响植被群落土壤侵蚀最重要的因素，乔灌木群落坡度 > 降雨量，草本群落降雨量 > 坡度。自然恢复植被群落枯落物盖度 > 植被盖度，人工植被群落植被盖度 > 枯落物盖度；因此，在当前植被条件下，未受到扰动的群落可有效减少降雨对土壤侵蚀的影响；在进行植被恢复时，应优先进行植被自然修复，适时适地引入乔灌木进行植被恢复人工调控，尽早促进乔木群落的林下植被发育，保护其林下灌草层和枯落物层，同时减少人为干扰。

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	赵珩钪
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关键词 ：土壤侵蚀, 植被群落, 侵蚀针法, 灰色关联分析, 黄土丘陵沟壑区

Abstract：[Background] The severe condition of soil and water loss in the Loess Plateau has resulted in critical agricultural and environmental problems. Vegetation restoration plays an essential role in controlling the soil erosion in the Loess Plateau. Yet there were few researches on analyzing the characteristics of soil erosion of different plant communities converted from slope cropland in the region. [Methods] The research was conducted between 2012 and 2015. Based on the succession of local plants, 10 plant communities on abandoned slope croplands in 4 watersheds of Ansai County were selected and were classified in 4 groups:naturally restored herbage community (Artemisia scoparia, Stipa bungeana, Bothriochloa ischaemun, Artemisia gmelinii, and Artemisia giraldii), naturally restored shrub community (Sophora viciifolia), artificially established shrub community (Caragana intermedia and Hippophae rhamnoides) and artificially established arbor community (Robinia psendoacacia and Populus simonii). Totally 45 plots were selected and in each of these communities 3-6 plots were selected, in each plot 3 quadrats were placed as repetition. Annual soil erosion intensity was monitored by erosion pins placed in these plots. Characteristics of soil erosion of different plant communities were analyzed with ANOVA, combined with the hydrologic years divided by the characteristics of rainfall. Gray theory was used to determine the influence of potential indices caused soil erosion. [Results] Rainfall in research area was distributed unevenly, and rainfall erosivity was the driver factor causing the differences of soil erosion intensity of plant communities in different years. The ability of controlling soil erosion depended on the species of plant community:naturally restored shrub community (1 285.36 t/km²) > naturally restored herbage community (2 152.65 t/km²) > artificially established shrub community(2 320.50 t/km²) > artificially established arbor community(2 661.14 t/km²). The soil erosion intensity of Robinia psendoacacia was the largest (3 875.02 t/km²) among these plant communities. Gray correlation analysis revealed that the rainfall and slope gradient had more impact on soil erosion than coverage in all communities. In shrub and arbor communities, the effect of slope gradient > rainfall, but in herbage communities, rainfall > slope gradient. When mentioned coverage, in natural restored community, cover of litters > vegetation cover; and in artificially established community, vegetation cover > cover of litters. [Conclusions] Under current status of vegetation, effects of precipitation on soil erosion reduced effectively in undisturbed plant communities. Natural vegetation should be restored initially with trees and shrubs introduced by human at proper time and place. Meanwhile, the undergrowth vegetation and litters in forest communities should be promoted earlier and protected, meanwhile human disturbances should be reduced as more as possible.

Key words： soil erosion plant communities erosion pin grey correlation analysis hilly-gully loess region

收稿日期: 2016-12-08

PACS:

S157

基金资助:国家自然科学基金"黄丘区坡面退耕与淤地坝对坡沟系统侵蚀产沙的阻控机理（41371280）"；水利部公益性行业科研专项经费项目"西北黄土高原区水土保持生态效应监测与评价技术研究"（201501045）

通讯作者: 焦菊英(1965-),女,研究员,博士生导师。主要研究方向:土壤侵蚀与植被关系及水土保持效益评价。E-mail:jyjiao@ms.iswc.ac.cn E-mail: jyjiao@ms.iswc.ac.cn

作者简介: 赵珩钪(1992-),男,硕士研究生。主要研究方向:土壤侵蚀。E-mail:zhkang1024@hotmail.com

引用本文:

赵珩钪¹, 曹斌挺², 焦菊英^1,3. 黄土丘陵沟壑区退耕坡地不同植物群落的土壤侵蚀特征[J]. 中国水土保持科学, 2017, 15(3): 105-113.
ZHAO Hengkang, CAO Binting, JIAO Juying. Characteristics of soil erosion of different plant communities converted from slope cropland in the hilly-gully region of the Loess Plateau. SSWC, 2017, 15(3): 105-113.

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http://journal12.magtechjournal.com/Jweb_stbc/CN/10.16843/j.sswc.2017.03.014 或 http://journal12.magtechjournal.com/Jweb_stbc/CN/Y2017/V15/I3/105

[1]	陈浩,蔡强国. 坡面植被恢复对沟道侵蚀产沙的影响[J]. 中国科学D辑:地球科学, 2006, 36(1):69. CHEN Hao, CAI Qiangguo. 坡面植被恢复对沟道侵蚀产沙的影响[J]. Science in China Series D:Earth Sciences, 2006, 36(1):69.
[2]	QIU L P, ZHANG X C, CHENG JM, et al. Effects of 22 years of revegetation on soil quality in the semi-arid area of the Loess Plateau[J]. African Journal of Biotechnology, 2009, 8(24):6896.
[3]	ZHANG L, DAWES W R, WALKER G R. Response of mean annual evapotranspiration to vegetation changes at catchment scale[J]. Water Resource Research, 2001, 37(3):701.
[4]	LIU Y, FU B, LYU Y, WANG Z, et al. Hydrological responses and soil erosion potential of abandoned cropland in the Loess Plateau, China[J]. Geomorphology, 2012, 138(1):404.
[5]	王晶, 朱清科, 秦伟, 等. 陕北黄土区封禁流域坡面微地形植被特征分异[J]. 应用生态学报, 2012, 23(3):694. WANG Jin, ZHU Qingke, QIN Wei, et al. Differentiation of vegetation characteristics on slope micro-topography of fenced watershed in loess area of North Shaanxi Province, Northwest China[J]. Chinese Journal of Applied Ecology, 2012, 23(3):694.
[6]	王世雄, 王孝安, 郭华. 黄土高原植物群落演替过程中的β多样性变化[J]. 生态学杂志, 2013,32(5):1135. WANG Shixiong, WANG Xiaoan, GUO Hua. Change patterns of β-diversity in the succession process of plant communities on the Loess Plateau of Northwest China[J]. Chinese Journal of Ecology, 2013, 32(5):1135.
[7]	焦菊英,张振国,贾燕锋,等.陕北丘陵沟壑区撂荒地自然恢复植被的组成结构与数量分类[J]. 生态学报,2008,28(7):2981. JIAO Juying, ZHANG Zhenguo, JIA Yanfeng, et al. Species composition and classification of natural vegetation in the abandoned lands of the hilly-gullied region of North Shaanxi Province[J]. Acta Ecologica Sinica, 2008, 28(7):2981.
[8]	赵冬, 许明祥, 刘国彬, 等. 用显微CT研究不同植被恢复模式的土壤团聚体微结构特征[J]. 农业工程学报, 2016, 32(9):123. ZHAO Dong, XU Mingxiang, LIU Guobin, et al. Characterization of soil aggregate microstructure under different re-vegetation types using micro-computed topography[J]. Transactions of the Chinese Society of Agricultural Engineering, 2016, 32(9):123.
[9]	冯天骄,卫伟,陈利顶,等.陇中黄土区坡面整地和植被类型对土壤化学性状的影响[J].生态学报,2016,36(11):3216. FENG Tianjiao,WEI Wei,CHENG Liding,et al. Effects of land preparations and vegetation types on soil chemical features in a loess hilly region[J].Acta Ecologica Sinica, 2016, 36(11):3216.
[10]	刘文祥, 李勇, 于寒青. 草灌植被恢复提高坡地土壤水稳性团聚体和碳、氮含量的有效性:退耕年限的影响[J]. 植物营养与肥料学报, 2016,22(1):164. LIU Wenxiang, LI Yong, YU Hanqing. Soil water stable aggregates and carbon and nitrogen storage enhanced by conversion of farmland to shrub and grass in China Loess Plateau:the influence of conversion cultivation time[J]. Journal of Plant Nutrition and Fertilizer, 2016,22(1):164.
[11]	刘洋, 黄懿梅, 曾全超. 黄土高原不同植被类型下土壤细菌群落特征研究[J/OL]. 环境科学, 2016(10):11[2016-12-02]. http://www.cnki.net/kcms/detail/11.1895.X.20160929.1347.035.html. LIU Yang, HUANG Yimei, ZENG Quanchao. Soil bacterial communities undet different vegetation types in the Loess Plateau[J/OL]. Environmental Science, 2016, (10):11[2016-12-02]. http://www.cnki.net/kcms/detail/11.1895.X.20160929.1347.035.html.
[12]	邢肖毅,黄懿梅,安韶山,等.黄土丘陵区不同植被土壤氮素转化微生物生理群特征及差异[J].生态学报,2013,33(18):5608. XING Xiaoyi,HUANG Yimei,AN Shaoshan, et al.Characteristics of physiological groups of soil nitrogen-transforming microbes in different vegetation types in the Loess Gully region,China[J].Acta Ecologica Sinica, 2013, 33(18):5608.
[13]	胡安,陈皓,陈先江,等.黄土高原农田与草原土壤种子库[J].草业科学,2015,32(7):1035. HU An, CHEN Hao, CHEN Xianjiang, et al.Soil seed banks of cropland and rangeland on the Loess Plateau[J]. Pratacultural Science, 2015, 32(7):1035.
[14]	朱智勇,解建仓,李占斌,等.坡面径流侵蚀产沙机理试验研究[J]. 水土保持学报, 2011. 25(5):1. ZHU Zhiyong, XIE Jiancang, LI Zhanbin, et al. Experimental study on mechanism of slope runoff-erosion sediment yield[J]. Journal of Soil Water Conservation, 2011, 25(5):1.
[15]	吕锡芝, 康玲玲, 左仲国, 等. 黄土高原吕二沟流域不同植被下的坡面径流特征[J]. 生态环境学报, 2015, 24(7):1113. LÜ Xizhi, KANG Lingling, ZUO Zhongguo, et al. Characteristics of slope runoff under different vegetation conditions in Lüergou Watershed of the Loess Plateau[J]. Ecology and Environmental Sciences, 2015, 24(7):1113.
[16]	易婷, 张光辉, 王兵, 等. 退耕草地近地表层特征对坡面流流速的影响[J]. 山地学报, 2015, 33(4):434. YI Ting, ZHANG Guanghui, WANG Bing, et al. Effects of near soil surface characteristics on velocity of overland flow in a natural succession grassland[J]. Mountain Research, 2015, 33(4):434.
[17]	刘栋,刘普灵,邓瑞芬,等. 不同下垫面径流小区次降雨侵蚀特征相关分析[J]. 水土保持通报, 2011, 31(2):99. LIU Dong, LIU Puling, DENG Ruifen, et al. Erosion characteristics of plots with various underlying surfaces in single rainfall[J]. Bulletin of Soil and Water Conservation, 2011, 31(2):99.
[18]	杨春霞,肖培青,甄斌,等.野外不同被覆坡面产流产沙特征[J]. 水土保持学报, 2012, 26(4):28. YANG Chunxia, XIAO Peiqing, ZHEN Bin, et al. Characteristics on runoff and sediment yield in field prototype and different coverage slope[J]. Journal of Soil and Water Conservation, 2012, 26(4):28.
[19]	徐佳,刘普灵,邓瑞芬, 等.黄土坡面不同植被恢复阶段的减流减沙效益研究[J]. 地理科学, 2012, (11):1391. XU Jia, LIU Puling, DENG Ruifen, et al. Runoff and sediment reductions in the different stages of vegetation restoration on a loess slope[J]. Scientia Geographica Sinica, 2012, (11):1391.
[20]	秦伟,朱清科,张宇清,赵磊磊. 陕北黄土区生态修复过程中植物群落物种多样性变化[J]. 应用生态学报,2009, 20(2):403. QIN Wei, ZHU Qingke, ZHANG Yuqing, et al. Dynamics of plant community species diversity in the process of ecological rehabilitation in North Shaanxi loess area[J]. Chinese Journal of Applied Ecology, 2009, 20(2):403.
[21]	焦菊英,张振国,贾燕锋,等. 陕北丘陵沟壑区撂荒地自然恢复植被的组成结构与数量分类[J]. 生态学报,2008,28(7):2981. JIAO Juying, ZHANG Zhenguo, JIA Yanfeng, et al. Species composition and classification of natural vegetation in the abandoned lands of the hilly-gullied region of North Shaanxi Province[J]. Acta Ecologica Sinica. 2008, 28(7):2981.
[22]	仝小林,李卫忠.延安市退耕还林工程林种、树种组成分析研究[J]. 陕西林业科技, 2007. 2:18. TONG Xiaolin, LI Weizhong. Research on forest category and species composition in the conversion of cropland to forest project in Yan'an Prefecture[J]. Shaanxi Forest Science and Technology, 2007, 2:18.
[23]	黄炎和,陈明华,黄鑫全. 土壤侵蚀量的标签定位测定法初探[J]. 福建水土保持, 1998(2):51. HUANG Yanhe, CHEN Minghua, HUANG Xinquan. 土壤侵蚀量的标签定位测定法初探[J]. Fujian Soil and Water Conservation, 1998(2):51.
[24]	章文波, 付金生. 不同类型雨量资料估算降雨侵蚀力[J]. 资源科学, 2003, 25(1):35. ZHANG Wenbo, FU Jinsheng. Rainfall erosivity estimation under different rainfall amount[J]. Resources Science, 2003, 25(1):35.
[25]	陶林威,马洪,葛芬莉. 陕西省降水特性分析[J]. 陕西气象, 2000(5):6. TAO Winwei, MA Hong, GE Fenli. 陕西省降水特性分析[J]. Journal of Shaanxi Meteorology, 2000(5):6.
[26]	邓聚龙. 灰色系统基本方法[M]. 武汉:华中理工大学出版社, 1987:33. DENG Julong. The primary methods of grey system theory[M]. Wuhan:Huazhong University of Science & Technology Press, 1987:33.
[27]	白文娟, 焦菊英, 马祥华, 等. 黄土丘陵沟壑区退耕地人工林的土壤环境效应[J]. 干旱区资源与环境, 2005, 19(7):135. BAI Wenjuan, JIAO Juying, MA Xianghua, et al. Soil environmental effects of artificial woods in abandoned croplands in the loess hilly-gullied region[J]. Journal of Arid Land Resources and Environment, 2005, 19(7):135.
[28]	李桂芳, 郑粉莉, 卢嘉, 等. 降雨和地形因子对黑土坡面土壤侵蚀过程的影响[J]. 农业机械学报, 2015,46(4):147. LI Guifang, ZHENG Fenli, LU Jia, et al. Effects of rainfall and topography on soil erosion processes of black soil hillslope[J]. Transactions of the Chinese Society for Agricultural Machinery, 2015, 46(4):147.
[29]	潘成忠, 上官周平.降雨和坡度对坡面流水动力学参数的影响[J]. 应用基础与工程科学学报, 2009, 17(6):843. PAN Chengzhong, SHANGGUAN Zhouping Experimental study on influence of rainfall land slope gradient on overland shallow flow hydraulics[J]. Journal of Basic Science and Engineering, 2009, 17(6):843.
[30]	沈海鸥, 郑粉莉, 温磊磊, 等. 降雨强度和坡度对细沟形态特征的综合影响[J]. 农业机械学报, 2015,46(7):162. SHEN Haiou, ZHENG Fenli, WEN Leilei, et al. Effects of rainfall intensity and slope gradient on rill morphological characteristics[J]. Transactions of the Chinese Society for Agricultural Machinery, 2015, 46(7):162.
[31]	杨帆,程金花,张洪江,等. 坡面草本植物对土壤分离及侵蚀动力的影响研究[J]. 农业机械学报, 2016, 47(5):129. YANG Fan, CHENG Jinhua, ZHENG Hongjiang, et al. Effect of herb plants on soil detachment and erosion dynamics[J]. Transactions of the Chinese Society for Agricultural Machinery, 2016, 47(5):129.
[32]	李鹏, 李占斌, 鲁克新. 黄土区草本植被根系与土壤垂直侵蚀产沙关系研究[J]. 植物生态学报, 2006, 30(2):302. LI Peng, LI Zhanbin, LU Kexin. Relationship between herbaceous root system and vertical soil sediment yield in loess area[J]. Journal of Plant Ecology, 2006, 30(2):302.
[33]	吴光艳, 成婧, 祝振华, 等. 黄土高原南部人工林林冠对降雨特征的影响分析[J]. 水土保持研究,2011,18(4):32. WU Guangyan, CHENG Jing, ZHU Zhenhua, et al. Rainfall characteristics under canopy of plantation forest in the southern Loess Plateau[J]. Research of Soil and Water Conservation, 2011, 18(4):32.
[34]	王冬, 杨政, 郝红敏,等. 黄土区退耕草地凋落物-土壤界面水分过程特征研究析[J]. 水土保持研究,2015, 22(1):80. WANG Dong, YANG Zheng, HAO Hongmin, et al. Hydrological processes of litter-soil interfacial systems in restoration grasslands of the loess region[J]. China. Research of Soil and Water Conservation,2015, 22(1):80.