东北黑土区农田防护林与沟谷侵蚀关系

doi:10.16843/j.sswc.2017.06.006

Abstract
Figure/Table
References (0)
Related Citation (15)

Download: PDF (2575 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract [Background] The black soil region in Northeast China is one of the most important marketable grain basis. The serious soil erosion brings crucial challenges to the production of marketable grain. Farmland shelterbelt is a key part of the Three Norths Forest Protection System in Northeast China, which plays a positive role in the prevention and control of soil erosion. The study on the effect of shelterbelt on gully can provide scientific insights into gully erosion control.[Methods] Firstly, the typical black soil region was chosen as the study area in Keshan County, Northeast China, and the distribution of gully and farmland shelterbelt was derived by interpreting the SPOT5 imagery in 2007 and TM imagery in 2008, respectively. Then, the effect of farmland shelterbelt on gully erosion was analyzed, using the spatial analysis and mathematical statistics methods.[Results] Generally, the density of farmland shelterbelts increased from northeast to southwest, while the variation law was the opposite for the density of gully. The highest density of farmland shelterbelt occurred in the western and northwestern regions, with the density larger than 1 400 m/km². And the highest density occurred in northeastern region for gully, >800 m/km². Furthermore, the defense effect of farmland shelterbelt on gully erosion varied with the defense distance. When the distance was shorter than 120 m, no obvious difference existed for the defense effect. When the distance ranged from 120 to 240 m, the defense effect decreased linearly with the increase of distance. When the distance was longer than 240 m, the defense effect decreased distinctly. Besides, the shelterbelt and gully density showed a highly linear relationship when the shelterbelt density ranged from 500 to 1 300 m/km². However, the change of gully density was not obvious when the shelterbelt density was higher than 1 300 m/km².[Conclusions] The slope, distance from the gully, and density of farmland shelterbelt were all import factors to the effect of farmland shelterbelt on gully erosion. The effect varied under different conditions of the three above mentioned factors. The farmland shelterbelt should be better planted in regions with the slope less than 8°, less than 120 m far away from the gully, and with the density ranging 1 100-1 300 m/km² in black soil region of Northeast China. This work may provide a certain scientific suggestion for the erosion prevention and management.

Key words： black soil region of Northeast China shelterbelts gully density gully erosion

Received: 13 October 2016

PACS:

S157.1

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	WANG Wenjuan
	DENG Rongxin
	HAO Lijun

Cite this article:

WANG Wenjuan,DENG Rongxin,HAO Lijun. Relationship between farmland shelterbelt and gully erosion in the black soil region of Northeast China[J]. SSWC, 2017, 15(6): 44-51.

URL:

http://journal12.magtechjournal.com/Jweb_stbc/EN/10.16843/j.sswc.2017.06.006 OR http://journal12.magtechjournal.com/Jweb_stbc/EN/Y2017/V15/I6/44

[1]	POEREN J, NACHTERGAELE J, VERSTRAETEN G, et al. Gully erosion and environmental change:importance and research needs[J]. Catena, 2003, 50(2-4):91.
[2]	KRAUSE A K, FRANKS S W, KALMA J D, et al. Multi-parameter fingerprinting of sediment deposition in a small gullied catchment in SE Australia[J]. Catena, 2003, 53(4):327.
[3]	沈波, 范建荣, 潘庆宾,等. 东北黑土区水土流失综合防治试点工程项目概况[J]. 中国水土保持,2003(11):7. SHEN Bo, FAN Jianrong, PAN Qingbin, et al. General situation of project for comprehensive control of soil erosion in black soil region of Northeast China[J]. China Soil and Water Conservation, 2003(11):7.
[4]	李和信,李忠辉,郑秀文.忍看黑土付流波?东北黑土区水土流失调查[R/OL].[2016-10-08]. http://www.people.com.cn/GB/huanbao/55/20020815/800101.html. LI Hexin,LI Zhenghui,ZHENG Xiuwen. Can see black soil pay flow? Survey of soil erosion in black soil region of Northeast China[R/OL].[2016-10-08]. http://www.people.com.cn/GB/huanbao/55/20020815/800101.html.
[5]	张永光,伍永秋,汪言在,等. 典型黑土区小流域浅沟侵蚀季节差异分析[J]. 地理研究, 2008,27(1):145. ZHANG Yongguang, WU Yongqiu, WANG Yanzai, et al. Seasonal discrepancy of ephemeral gully erosion in Northeast China with black soils[J]. Geographical Research, 2008, 27(1):145.
[6]	孟令钦, 李勇.东北黑土区坡耕地侵蚀沟发育机理初探[J].水土保持学报,2009, 23(1):7. MENG Lingqin, LI Yong. The Mechanism of gully development on sloping farmland in black soil area, Northeast China[J]. Journal of Soil and Water Conservation, 2009, 23(1):7.
[7]	ZHANG Y G, WU Y Q, LIU B Y, et al. Characteristics and factors controlling the development of ephemeral gullies in cultivated catchments of black soil region, Northeast China[J]. Soil & Tillage Research, 2007(9):28.
[8]	WU Y Q, ZHENG Q H, ZHANG Y G, et al. Development of gullies and sediment production in the black soil region of northeastern China[J]. Geomorphology, 2008(101):683.
[9]	董一帆, 伍永秋.利用虚拟插钎对切沟沟底不同部位短期变化的初步研究[J].地理科学,2010, 30(6):892. DONG Yifan,WU Yongqiu. Short-term gully erosion at different places of bottom of gully using virtual erosion pins[J]. Scientia Geographica Sinicae, 2010, 30(6):892.
[10]	王文娟,张树文,方海燕. 东北典型黑土区坡沟侵蚀耦合关系[J]. 自然资源学报, 2012, 27(12):2113. WANG Wenjuan, ZHANG Shuwen,FANG Haiyan. Coupling mechanism of slope-gully system in type black soil area of Northeast China[J]. Journal of Natural Resources, 2012,27(12):2113.
[11]	王文娟, 邓荣鑫, 张树文. 东北典型黑土区40年来沟蚀空间格局变化及地形分异规律[J]. 地理与地理信息科学,2012, 28(3):68. WANG Wenjuan, DENG Rongxin, ZHANG Shuwen. Spatial pattern change and topographic differentia of gully erosion in the type black soil area of Northeast China during the past 40 years[J]. Geography and Geo-Information Science, 2012,28(3):68.
[12]	闫业超,张树文,岳书平. 近40 a黑土典型区坡沟侵蚀动态变化[J]. 农业工程学报,2010,26(2):109. YAN Yechao, ZHAN Shuwen, YUE Shuping. Dynamic change of hill slope and gully erosion in typical area of black soil region during the past 40 years[J]. Transactions of the CSAE, 2010,26(2):109.
[13]	SHI C T, Wang E H, GU H Y,et al.Soil structure characters of different soil and water conservation plantations in typical black soil region[J].Journal of Forestry Research,2010(21):151.
[14]	陈平,万福绪,唐晓岚,等. 苏州市胥口镇城郊防护林规划研究[J]. 北京林业大学学报(社会科学版),2010,3(1):90. CHEN Ping,WAN Fuxu,TANG Xiaolan,et al.Planning of suburban shelter forest in Xukou Town of Suzhou City[J].Journal of Beijing Forestry University (Social Sciences), 2010,3(1):90.
[15]	马浩,周志翔,王鹏程,等. 基于多目标灰色局势决策的三峡库区防护林类型空间优化配置[J]. 应用生态学报,2010,21(12):3083. MA Hao,ZHOU Zhixiang,WANG Pengcheng,et al.Spatial optimum allocation of shelterforest types in Three Gorges Reservoir Area based on multiple objective grey situation decision[J].Chinese Journal of Applied Ecology,2010,21(12):3083.
[16]	WANG X M, ZHANG C X, HASI E, et al. Has the Three Norths Forest Shelterbelt Program solved the desertification and dust storm problems in arid and semiarid China[J]. Journal of Arid Environments, 2010(74):13
[17]	苏子龙,崔明,范昊明. 基于东北漫岗黑土区坡耕地沟蚀防治的防护林带布局优化[J]. 应用生态学报,2012,23(4):903. SU Zilong,CUI Ming,FAN Haoming. Optimization of shelterbelt distribution for the gully erosion control of cultivated slope land in rolling hill black soil region of Northeast China[J].Chinese Journal of Applied Ecology, 2012,23(4):903.
[18]	苏子龙,崔明,范昊明. 东北漫岗黑土区防护林带分布对浅沟侵蚀的影响[J]. 水土保持研究,2012,19(3):20. SUZilong,CUI Ming,FAN Haoming. Effect of shelbelts distribution on ephemeral gully erosion in the rolling hill black soil region of Northeast China[J]. Research of Soil and Water Conservation 2012,19(3):20.
[19]	闫业超,张树文,岳书平.克拜东部黑土区侵蚀沟遥感分类与空间格局分析.地理科学,2007,27(2):193. YAN Yechao, ZHANG Shuwen, YUE Shuping. Classification of erosion gullies by remote sensing and spatial pattern analysis in black soil region of eastern Kebai[J]. Scientia Geographica Sinica, 2007,27(2):193.
[20]	范志平, 曾德慧, 陈伏生, 等. 2004. 东北地区农田防护林结构对林网内积雪分布格局的影响[J]. 应用生态学报, 2004,15(2):181. FAN Zhiping, ZENG Dehui, CHEN Fusheng, et al. Influence of shelterbelts structure on snow distribution pattern in shelternets in Northeast China[J]. Chinese Journal of Applied Ecology, 2004, 15(2):181.
[21]	范志平, 曾德慧, 朱教君, 等. 农田防护林生态作用特征研究[J]. 水土保持学报, 2002, 16(4):130. FAN Zhiping, ZENG Dehui, ZHU Jiaojun, et al. Advance in characteristics of ecological effects of farmland shelterbelts[J]. Journal of Soil and Water Conservation, 2002, 16(4):130.
[22]	郝宏. 黑龙江省西部防护林体系优化模式研究[D].哈尔滨:东北林业大学,2001:9. HAO Hong. Study on the optimal model of protective forest system in the west region of Heilongjiang Province[D]. Northeast Forestry University, 2001:9.
[23]	王文彪,党晓宏,张吉树,等. 库布齐沙漠北缘不同作物秸秆平铺式沙障的防风效能[J].中国沙漠, 2013,33(1):65. WANG Wenbiao,DANG Xiaohong,ZHANG Jishu,et al. The wind-breaking efficiency of low vertical sand barriers with different materials in northern edge of Hobq desert[J].Journal of Desert Research, 2013,33(1):65.
[24]	高函, 吴斌, 张宇清, 等.行带式配置柠条林防风效益风洞试验研究[J]. 水土保持学报,2010, 24(4):44. GAO Han, WU Bin, ZHANG Yuqing et al. Wind tunnel test of wind speed reduction of Caragana korshinskii Coppice[J]. Journal of Soil and Water Conservation, 2010, 24(4):44.
[25]	查同刚,孙向阳,于卫平,等. 宁夏地区农田防护林结构与小气候效应[J]. 中国水土保持科学, 2004, 2(4):82. ZHA Tonggang,SUN Xiangyang,YU Weiping,et al. Structure and microclimate effects of shelterbelt on farmland in Ningxia[J]. Science of Soil and Water Conservation, 2004, 2(4):82.
[26]	徐海, 夏焕柏. 乌江流域坡耕地水保防护林体系建设技术研究[J]. 土壤侵蚀与水土保持学报,1997, 11(3):17. XU Hai,XIA Huanbai. Study on structure technique of protecting forest system on sloping field in Wujiang river watershed[J]. Journal of Soil Erosion and Soil and Water Conservation, 1997, 11(3):17.
[27]	欧阳君祥. 内蒙古赤峰市退化防护林改造更新研究[J]. 中南林业科技大学学报,2015,35(9):1. OUYANG Junxiang. Reform and regeneration of degenerative shelter-forest in Inner Mongolia Chifeng[J]. Journal of Central South University of Forestry & Technology,2015,35(9):1.
[28]	孙尚海, 张淑芝. 应用耗散结构理论配置水保林体系及其效益研究[J]. 中国水土保持,1995(4):23. SUN Shanghai, ZHANG Shuzhi. Application of dissipative structure theory on configuration of water and conservation shelterbelt system and study on its benefit[J]. China Soil and Water Conservation, 1995(4):23.