Soil Water Redistribution Pattern of Caragana intermedia Hedgerow System in Semi-arid Area

DANG Han-jin; DANG Hong-zhong; WANG Yu-kui; ZHOU Ze-fu

Volume 27 Issue 6

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Soil Water Redistribution Pattern of Caragana intermedia Hedgerow System in Semi-arid Area

1.
China National Bamboo Research and Development Center, Chinese Academy of Forestry, Hangzhou 310012, Zhejiang, China
2.
Institute of Desertification Studies, Chinese Academy of Forestry, Beijing 100091, China

Received Date: 2013-04-27

Abstract

The soil moisture contents at four locations (inter-band, front-band, inner-band and behind-band) of Caragana intermedia hedgerow system which was located in the hilly area of Loess Plateau were measured for 2 years. The results indicated that there were obvious differences in soil water physical properties among locations. The soil bulk density(0.99 g·cm-3), non-capillary porosity(8.77%) and capillary moisture capacity(58.89 %) of inner-band were better than the other parts of the system with looser soil and higher soil water permeability and water retention. The soil of front-band was stickier than that of the others. The soil moisture content of each position decreased by the order 0-20 cm (25.51%±2.28%) > 40-60 cm (12.96%±1.34%) > 60-80 cm (10.03%±0.59%) > 80-100 cm (9.16%±0.81%) > 100-120 cm (8.76%±1.00%) with depths, for the surface layer, the soil moisture contents of the front-band and inner-band were higher than that of the others. The profile of soil moisture of hedgerow system were divided into three layers based on the orderly cluster analysis of soil moisture, namely, weak moisture utilizing layer, moisture utilizing layer, and moisture regulating layer. The depth of moisture utilizing layer of inner-band soil (20-120 cm) was greater than that of front-band, behind-band (20-60 cm) and inter-band (40-60 cm), similarly, the moisture regulating layer of inner-band soil (below 120 cm) was deeper than that of inter-band (below 80 cm), front-band (below 60 cm) and behind-band (below 60 cm), too, which reflected the effects of runoff intercepting, enriching soil moisture to the inner-band, high infiltration and reservoir of hedgerow system.
- semi-arid area,
- Caragana intermedia,
- hedgerow,
- soil moisture,
- soil water redistribution

References

[1]	杨承栋. 论合理保护开发利用中国森林土壤资源[J]. 世界林业研究,2011,24(1):19-27.
[2]	朱显谟. 抢救"土壤水库"实为黄土高原生态环境综合治理与可持续发展的关键——四论黄土高原国土整治28字方略[J]. 水土保持学报,2000,14(1):1-6.
[3]	Galle S,Ehrmann M,Peugeot C. Water balance in a banded vegetation pattern:A case study of tiger bush in western Niger[J]. Catena,1999,37(1-2):75-88.
[4]	Lefever R,Lejeune O. On the origin of tiger bush[J]. Bulletin of mathematical biology,1997,59(2):263-294.
[5]	Dercon G,Decjers J,Posen J,et al. Spatial variability in crop response under contour hedgerow systems in the Andes region of Ecuador[J]. Soil and tillage research,2006,86(1):15-26.
[6]	唐政洪,蔡强国,许峰,等. 半干旱区植物篱侵蚀及养分控制过程的试验研究[J]. 地理研究,2001,20(5):593-600.
[7]	王正秋. 等高灌木带是坡耕地治理的重要技术措施[M]. 北京:中国环境科学出版社,1995: 190-198.
[8]	申元村. 三峡库区植物篱坡地农业技术水土保持效益研究[J]. 土壤侵蚀与水土保持学报,1998,4(2):61-66
[9]	蔡强国,黎四龙. 植物篱笆减少侵蚀的原因分析[J]. 土壤侵蚀与水土保持学报,1988,4(2):54-60.
[10]	Dano M A. 菲律宾陡坡耕地水土保持措施的效益[J]. 水土保持科技情报,1993(4):52-54.
[11]	蔡强国,吴淑安,马绍喜. 三峡库区坡地改良利用[M]. 北京:中国环境科学出版社,1995: 305-309.
[12]	郑度,申元村. 坡地过程及退化坡地恢复整治研究——以三峡库区紫色土坡地为例[J]. 地理学报,1998,53(2):116-122.
[13]	Majed A Z. Factors affecting sediment trapping in vegetated filter strips:simulation study using VFSMOD[J]. Hydrological processes,2001,15(8):1477-1488.
[14]	Esteban J,Fairen V. Self-organized formation of banded vegetation patterns in semi-arid regions:A model[J]. Ecological complexity,2006,3(2):109-118.
[15]	Bryan R B,Brun S E. Laboratory experiments on sequential scour/deposition and their application to the development of banded vegetation[J]. Catena,1999,37(1-2):147-163.
[16]	李俊,毕华兴,李笑吟,等. 有序聚类法在土壤水分垂直分层中的应用[J]. 北京林业大学学报,2007,29(1):98-101.
[17]	王信增,焦峰. 基于有序聚类法的土壤水分剖面划分[J]. 西北农林科技大学学报:自然科学版,2011,39(2):191-201.
[18]	陈洪松,邵明安. 黄土区坡地土壤水分运动与转化机理研究进展[J]. 水科学进展,2003,14(4):513-520.
[19]	余新晓,张建军,朱金兆. 黄土地区防护林生态系统土壤水分条件的分析与评价[J]. 林业科学,1996,32(4):289-297
[20]	卜崇峰,蔡强国,袁再健. 三峡库区等高植物篱的控蚀效益及其机制[J]. 中国水土保持科学,2006,4(4):14-18.
[21]	孙辉,唐亚,陈克明等. 等高固氮植物篱控制坡耕地地表径流的效果 [J]. 水土保持通报,2001,21(2):48-51.
[22]	卜崇峰,蔡强国,袁再健. 湿润区坡耕地香根草植物篱农作措施对土壤侵蚀和养分的影响[J]. 农业工程学报,2006,22(5):55-60.
[23]	段建军,王小利,张彩霞.黄土高原土壤干层评定指标的改进及分级标准[J]. 水土保持学报,2007,21(6):151-154.
[24]	王国梁,刘国彬,周生路.黄土高原土壤干层研究述评[J]. 水土保持学报,2003,17(6):156-159.
[25]	Lefever R,Lejeune O. On the origin of tiger bush[J]. Bulletin of mathematical biology,1997,59(2):263-294.
[26]	Bryan R B,Brun S E. Laboratory experiments on sequential scour/deposition and their application to the development of banded vegetation[J]. Catena,1999,37(1-2):147-163.
[27]	Ludwig J A,Tongway D J,Marsden S G. Stripes,strands or stipples:modeling the influence of three landscape banding patterns on resource capture and productivity in semi-arid woodlands,Australia[J]. Catena,1999,37(1-2):257-273.

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通讯作者: 陈斌, bchen63@163.com

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沈阳化工大学材料科学与工程学院沈阳 110142

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Soil Water Redistribution Pattern of Caragana intermedia Hedgerow System in Semi-arid Area

1. China National Bamboo Research and Development Center, Chinese Academy of Forestry, Hangzhou 310012, Zhejiang, China

2. Institute of Desertification Studies, Chinese Academy of Forestry, Beijing 100091, China

Received Date: 2013-04-27

Abstract: The soil moisture contents at four locations (inter-band, front-band, inner-band and behind-band) of Caragana intermedia hedgerow system which was located in the hilly area of Loess Plateau were measured for 2 years. The results indicated that there were obvious differences in soil water physical properties among locations. The soil bulk density(0.99 g·cm-3), non-capillary porosity(8.77%) and capillary moisture capacity(58.89 %) of inner-band were better than the other parts of the system with looser soil and higher soil water permeability and water retention. The soil of front-band was stickier than that of the others. The soil moisture content of each position decreased by the order 0-20 cm (25.51%±2.28%) > 40-60 cm (12.96%±1.34%) > 60-80 cm (10.03%±0.59%) > 80-100 cm (9.16%±0.81%) > 100-120 cm (8.76%±1.00%) with depths, for the surface layer, the soil moisture contents of the front-band and inner-band were higher than that of the others. The profile of soil moisture of hedgerow system were divided into three layers based on the orderly cluster analysis of soil moisture, namely, weak moisture utilizing layer, moisture utilizing layer, and moisture regulating layer. The depth of moisture utilizing layer of inner-band soil (20-120 cm) was greater than that of front-band, behind-band (20-60 cm) and inter-band (40-60 cm), similarly, the moisture regulating layer of inner-band soil (below 120 cm) was deeper than that of inter-band (below 80 cm), front-band (below 60 cm) and behind-band (below 60 cm), too, which reflected the effects of runoff intercepting, enriching soil moisture to the inner-band, high infiltration and reservoir of hedgerow system.

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Reference (27)

[1]	杨承栋. 论合理保护开发利用中国森林土壤资源[J]. 世界林业研究,2011,24(1):19-27.
[2]	朱显谟. 抢救"土壤水库"实为黄土高原生态环境综合治理与可持续发展的关键——四论黄土高原国土整治28字方略[J]. 水土保持学报,2000,14(1):1-6.
[3]	Galle S,Ehrmann M,Peugeot C. Water balance in a banded vegetation pattern:A case study of tiger bush in western Niger[J]. Catena,1999,37(1-2):75-88.
[4]	Lefever R,Lejeune O. On the origin of tiger bush[J]. Bulletin of mathematical biology,1997,59(2):263-294.
[5]	Dercon G,Decjers J,Posen J,et al. Spatial variability in crop response under contour hedgerow systems in the Andes region of Ecuador[J]. Soil and tillage research,2006,86(1):15-26.
[6]	唐政洪,蔡强国,许峰,等. 半干旱区植物篱侵蚀及养分控制过程的试验研究[J]. 地理研究,2001,20(5):593-600.
[7]	王正秋. 等高灌木带是坡耕地治理的重要技术措施[M]. 北京:中国环境科学出版社,1995: 190-198.
[8]	申元村. 三峡库区植物篱坡地农业技术水土保持效益研究[J]. 土壤侵蚀与水土保持学报,1998,4(2):61-66
[9]	蔡强国,黎四龙. 植物篱笆减少侵蚀的原因分析[J]. 土壤侵蚀与水土保持学报,1988,4(2):54-60.
[10]	Dano M A. 菲律宾陡坡耕地水土保持措施的效益[J]. 水土保持科技情报,1993(4):52-54.
[11]	蔡强国,吴淑安,马绍喜. 三峡库区坡地改良利用[M]. 北京:中国环境科学出版社,1995: 305-309.
[12]	郑度,申元村. 坡地过程及退化坡地恢复整治研究——以三峡库区紫色土坡地为例[J]. 地理学报,1998,53(2):116-122.
[13]	Majed A Z. Factors affecting sediment trapping in vegetated filter strips:simulation study using VFSMOD[J]. Hydrological processes,2001,15(8):1477-1488.
[14]	Esteban J,Fairen V. Self-organized formation of banded vegetation patterns in semi-arid regions:A model[J]. Ecological complexity,2006,3(2):109-118.
[15]	Bryan R B,Brun S E. Laboratory experiments on sequential scour/deposition and their application to the development of banded vegetation[J]. Catena,1999,37(1-2):147-163.
[16]	李俊,毕华兴,李笑吟,等. 有序聚类法在土壤水分垂直分层中的应用[J]. 北京林业大学学报,2007,29(1):98-101.
[17]	王信增,焦峰. 基于有序聚类法的土壤水分剖面划分[J]. 西北农林科技大学学报:自然科学版,2011,39(2):191-201.
[18]	陈洪松,邵明安. 黄土区坡地土壤水分运动与转化机理研究进展[J]. 水科学进展,2003,14(4):513-520.
[19]	余新晓,张建军,朱金兆. 黄土地区防护林生态系统土壤水分条件的分析与评价[J]. 林业科学,1996,32(4):289-297
[20]	卜崇峰,蔡强国,袁再健. 三峡库区等高植物篱的控蚀效益及其机制[J]. 中国水土保持科学,2006,4(4):14-18.
[21]	孙辉,唐亚,陈克明等. 等高固氮植物篱控制坡耕地地表径流的效果 [J]. 水土保持通报,2001,21(2):48-51.
[22]	卜崇峰,蔡强国,袁再健. 湿润区坡耕地香根草植物篱农作措施对土壤侵蚀和养分的影响[J]. 农业工程学报,2006,22(5):55-60.
[23]	段建军,王小利,张彩霞.黄土高原土壤干层评定指标的改进及分级标准[J]. 水土保持学报,2007,21(6):151-154.
[24]	王国梁,刘国彬,周生路.黄土高原土壤干层研究述评[J]. 水土保持学报,2003,17(6):156-159.
[25]	Lefever R,Lejeune O. On the origin of tiger bush[J]. Bulletin of mathematical biology,1997,59(2):263-294.
[26]	Bryan R B,Brun S E. Laboratory experiments on sequential scour/deposition and their application to the development of banded vegetation[J]. Catena,1999,37(1-2):147-163.
[27]	Ludwig J A,Tongway D J,Marsden S G. Stripes,strands or stipples:modeling the influence of three landscape banding patterns on resource capture and productivity in semi-arid woodlands,Australia[J]. Catena,1999,37(1-2):257-273.

Soil Water Redistribution Pattern of Caragana intermedia Hedgerow System in Semi-arid Area

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通讯作者: 陈斌, bchen63@163.com

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Soil Water Redistribution Pattern of Caragana intermedia Hedgerow System in Semi-arid Area

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