[1]严冬春,文安邦,龚长文,等.紫色土陡坡耕地顺坡垄作条件下的土壤及其流失特征[J].山地学报,2014,(03):314.
 YAN Dongchun,WEN Anbang,GONG Changwen,et al.Characteristics of Purple Soil and Soil Loss on Downslope Furrow Tillage Sloping Farmland[J].Mountain Research,2014,(03):314.
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紫色土陡坡耕地顺坡垄作条件下的土壤及其流失特征()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2014年03期
页码:
314
栏目:
山地研究
出版日期:
2014-03-01

文章信息/Info

Title:
Characteristics of Purple Soil and Soil Loss on Downslope Furrow Tillage Sloping Farmland
作者:
严冬春文安邦龚长文袁雪峰
1.中国科学院水利部成都山地灾害与环境研究所,山地表生过程与生态调控重点实验室,四川 成都 610041;
2.重庆市忠县水务局,重庆 忠县 404300
Author(s):
YAN Dongchun WEN Anbang GONG Changwen YUAN Xuefeng(319)
1. Key Laboratory of Mountain Environment Evolvement and Regulation, Institute of Mountain Hazards and Environment, CAS, No. 9, block 4, South Renmin Road, Chengdu, Sichuan 610041, China;
2. Water Authority of Zhongxian County, Zhongxian, Chongqing 404300, China
关键词:
紫色土陡坡耕地顺坡垄作水土保持
Keywords:
purple soil sloping farmland downslope furrow tillage soil and water conservation
分类号:
S155.2+5,S157.1
文献标志码:
A
摘要:
顺坡垄作是在长江上游特别是紫色土坡耕地上农民普遍采用的耕作模式,以往由于主流思想的影响,没有得到应有的重视。以三峡库区紫色土坡耕地为例,采用野外调查与小区实验相结合,分别采集垄沟和垄坡表层土壤,测试顺坡垄作地块沟、垄土壤容重、粒径分布、有机质含量、TN、TP、土壤含水量等指标,小区实验调查顺坡垄作条件下的土壤流失特征,进而探讨顺坡垄作导致的土壤特性差异与顺坡垄作的水土保持机制。结果表明:与垄沟内土壤相比,垄坡土壤平均含水量、容重分别降低2974 %和1641 %,土壤总孔隙度高2056%,说明垄坡土壤具有更大的吸持水分的潜力,降雨产流阈值相比于垄沟土壤也更大。相比于垄沟内土壤,粘粒在垄沟内发生富集,垄坡土壤中的有机质、总氮(TN)和总磷(TP)指标分别高1879 %、1730 %和931 %。侵蚀泥沙中沙粒含量出现明显富集,几乎是垄沟土壤沙粒含量的1倍,而粘粒和粉粒含量则远小于径流小区土壤成分,说明顺坡垄作有利于<50 μm土壤细颗粒的保持。侵蚀泥沙中有机质和TN远小于径流小区土壤成分,而TP则高于径流小区土壤成分,与侵蚀泥沙颗粒分选现象近似,说明顺坡垄作的肥力指标流失差异同样主要由侵蚀分选导致,也说明顺坡垄作有利于紫色土有机质和氮肥的保持。
Abstract:
Although downslope tillage was used to practice on purple soil sloping farmland in the upper reach of Yangtze River, fewer details were investigated in past decades. This study focus on downslope tillage on purple soil sloping farmland in the Three Gorges Reservoir Regions, the field investigate method and runoff plot method were utilized to survey scales of downslope furrow, soil density, soil particle distribution, TOC, TN, TP and water content. The results displayed that, compared with downslope furrow, soil water content and soil density in the furrow slope were less than 29.74% and 16.41%, but the soil total porosity was more than 20.56%. Clay particles were enriched in the downslope furrows, the TOC, TN and TP contents in furrow slope soil were more than 18.79%, 17.30% and 9.31%, respectively. Sand particles were enriched double in sediment, but clay particles and silt particles contents in sediment were less compared with plot soil, it was implied that the downslope furrow tillage method contributed >50μm fine particles to be conservation. TOC and TN contents in sediment were fewer than in the plot soil, and this trend was similar to fine particles, it was illustrated the downslope furrow tillage method contributed TOC and TN conservation too.

参考文献/References:

[1] Yang Zisheng. Review of study on soil erosion of sloping cultivated land and its sustainable use in the northeast mountain region of Yunnan province of the upper Yangtze river [J]. Mountain Research, 1999, 17(5): 1-5[杨子生.长江上游滇东北山区坡耕地水土流失与可持续利用研究简介[J]. 山地学报, 1999, 17(5): 1-5]
[2] Wang Ji, Wang Shijie, Chen Xi,et al. Research of the application of agronomic techniques for water and soil preservation in hilly regions [J]. Journal of Southwest Agricultural University :Natural Science,2003, 25(6): 530-534[王济, 王世杰, 陈曦, 等. 旱坡地水土保持耕作技术应用的研究[J]. 西南农业大学学报:自然科学版,2003, 25(6): 530-534]
[3] Wang Yongqiang, Wang Yukuan, Fu Bin,et al. Study of soil erosion in areas of purple soil under various cultivation systems [J]. Research of Soil and Water Conservation, 2007,14(3):333-335[王勇强,王玉宽,付斌,等.不同耕作方式对紫色土侵蚀的影响[J].水土保持研究,2007,14(3):333-335]
[4] Liu Gangcai, Gao Meirong, Lin Sanyi,et al. Process characteristics of soil and water Loss under two tillage systems and valuation of measurement for soil erosion [J]. Journal of Soil and Water Conservation, 2002,16(4):108-111[刘刚才,高美荣,林三益,等. 紫色土两种耕作制的产流产沙过程与水土流失观测准确性分析[J].水土保持学报,2002,16(4):108-111]
[5] Yan Dongchun, Long Yi, Shi Zhonglin. Downslope furrow tillage system in the upper reach of Yangtze River [J]. Soil and Water Conservation in China,2010,10:8-9[严冬春,龙翼,史忠林. 长江上游陡坡耕地“大横坡+小顺坡”耕作模式[J]. 中国水土保持,2010,10:8-9]
[6] Zhu Bo, Kuang Fuhong, Gao Meirong,et al. Effects of soil thickness on productivity of sloping cropland of purple soil [J]. Mountain Research, 2009,27(6):735-739[朱波,匡福虹,高美荣,等. 土层厚度对紫色土坡地生产力的影响[J]. 山地学报,2009,27(6):735-739]
[7] Guo Jin, Wen Anbang, Yan Dongchun,et al. Particle characteristics of eroded purple soil from slope land in the Three Gorges Reservoir Region [J]. Journal of Soil and Water Conservation, 2012,26(3):18-21[郭进,文安邦,严冬春,等. 三峡库区紫色土坡地土壤颗粒流失特征[J]. 水土保持学报,2012,26(3):18-21]

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备注/Memo

备注/Memo:
收稿日期(Received date):2013-07-16;改回日期(Accepted): 2013-10-21。
基金项目(Foundation item):国家自然科学基金(课题号:41201275),国家科技支撑计划项目(课题号:2011BAD31B03),中国科学院西部行动计划(课题号:KZCX2-XB3-09)。[National natural science foundation of China (No. 41201275), Science and technology support project in China (No. 2011BAD31B03), CAS Western Project(No. KZCX2-XB3-09).]
作者简介(Biography):严冬春,男,1981年出生,湖北宜昌人,博士,主要从事土壤侵蚀与水土保持研究。[Yan Dongchun, male, come from Yichang and was born in 1981, Ph D, mostly engage soil erosion and soil and water conservation study.] Tel: 13438382030, E-mail: yandc@imde.ac.cn
更新日期/Last Update: 1900-01-01