土地利用

生态重建模式的评价方法——以黄土丘陵区为例

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  • 1. 中国科学院地理科学与资源研究所,北京 100101;
    2. 中国科学院水土保持研究所,陕西杨凌 712100
徐勇 (1964-), 男, 陕西榆林人, 副研究员。主要从事农业与乡村发展、土地利用变化与可持续发展等领域的科研工作。E-mail:yongxu@sina.com

收稿日期: 2003-11-10

  修回日期: 2004-03-22

  网络出版日期: 2004-07-25

基金资助

国家自然科学基金项目 (40371051);中国科学院知识创新工程项目 (KZCX1-6-2-6)

The Evaluating Method of Eco-environment Restoration Patterns: A Case Study of the Loess Hilly-gully Region

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  • 1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
    2. Institute of Soil and Water Conservation Research, CAS, Yangling Shaanxi 712100, China

Received date: 2003-11-10

  Revised date: 2004-03-22

  Online published: 2004-07-25

Supported by

National Natural Science Foundation of China, No.40371051; Knowledge Innovation Project of CAS, No.KZCX1-6-2-6

摘要

生态重建模式是协调生态脆弱地区人地关系的系列政策和配套措施的总称。作者在按模式总体特征、生态重建规模、投资需求及实施效果开展评价方法讨论和筛选评价指标的基础上,以黄土丘陵区为例,总结了“赈济退耕”、“梯田退耕”和“坝系根治”3种模式的基本特征,计算了不同模式下黄土丘陵区生态重建关于退耕、新修梯田、园地扩建、建坝淤地以及林草植被恢复等的规模和投资需求额度,分析了各模式下的生态重建效益。结果表明:“梯田退耕”可作为黄土丘陵区生态重建的主体模式,目前正在实施的“赈济退耕”具有显著的过渡性特征,“坝系根治”在局部区域可作为辅助模式。

本文引用格式

徐勇,田均良,沈洪泉,刘普灵 . 生态重建模式的评价方法——以黄土丘陵区为例[J]. 地理学报, 2004 , 59(4) : 621 -628 . DOI: 10.11821/xb200404017

Abstract

The eco-environment restoration pattern means an integration of the policies and their matching measures in regulating the relation between human being and environment in the eco-environmentally fragile areas. This paper discussed the contents, indices and methods of the pattern evaluation. And then, based on the research results in the past ten years and the successful cases of small watersheds in the loess hilly-gully region, the characteristics of eco-environment restoration patterns including "relieving and de-farming" (RD), "rebuilding terrace and de-farming" (RTD) and "dam system and permanent control" (DSPC) were summarized. The sizes of de-farming slope farmland, rebuilding terrace, enlarging garden plot and restoring vegetation were calculated, the investment demands of eco-environment restoration on three patterns were done, benefits from those patterns were analyzed respectively and compared among each other. As a result, this paper drew the following conclusions: (1) RD pattern showed that the area of de-farming slope farmland more than 25o is 41.91×104 hm2 with 44.01×108 yuan (RMB) of policy allowance, and that of de-farming slope farmland more than 15o is 125.53×104 hm2 with 131.82×108 yuan of that. The result of RTD pattern is that the area of enlarged terraces is 69.16×104 hm2 and that of restored vegetation is 541.02×104 hm2, with 125.05×108 yuan of total investment demand. And the data from DSPC pattern included 36×104 silt-covered dams, 55.98×104 hm2 of silt-covered farmland and 554.2×104 hm2 of new woodland or grassplot, and 221.22×108 yuan of investment demand. (2) The benefit analysis of three patterns and their comparison results showed that RTD pattern ranks the first, with appropriate investment demand, better benefit and safer food supplies. Compared with RTD, RD being underway at present is a transitional pattern, with lower benefit and unsafe food supplies, and it should be replaced with RTD as soon as possible. On account of the limitation of its bigger investment demand and more uncertain factors, DSPC can be only regarded as an accessorial pattern, in despite of its profit prior to that of RTD.

参考文献


[1] Tian Junliang, Liang Yimin, Liu Puling (eds.). Research on Eco-agriculture Construction of Meso-scale Area in the Loess Hilly-Gully Region. Zhengzhou: Yellow River Water Conservancy Press, 2003.

[2] Xu Jiongxin. Some problems and research requirements concerning eco-environmental construction on Loess Plateau. Research of Soil and Water Conservation, 2000, 7(2): 10-13.
[许炯心. 黄土高原生态环境建设的若干问题与研究需求. 水土保持研究, 2000, 7(2): 10-13.]

[3] Jing Ke. On the construction of ecological agriculture in the middle of the Loess Plateau. Geographical Research, 1999, 18(s): 51-56.
[景可. 黄土高原中部生态农业建设探讨. 地理研究, 1999, 18(s): 51-56.]

[4] Kang Xiaoguang. Dam system agriculture is the basis of harnessing the Yellow River. Science & Technology Review, 1993, 62(8): 3-6.
[康晓光. 坝系农业--治黄之本. 科技导报, 1993, (8): 3-6.]

[5] Xu Yong, Roy C Sidle. Research on land use change and its regulation of Yangou Watershed in loess hilly-gully region. Acta Geographica Sinica, 2001, 56(6): 681-710.
[徐勇, Roy C Sidle. 黄土丘陵区燕沟流域土地利用变化与优化调控. 地理学报, 2001, 56(6): 681-710.]

[6] Fu Bojie, Chen Liding, Ma Keming. The effect of land use change on the regional environment in the Yangjuangou Catahment in the Loess Plateau of China. Acta Geographica Sinica, 2001, 54(3): 241-246.
[傅伯杰, 陈利顶, 马克明. 黄土丘陵区小流域土地利用变化对生态环境的影响--以延安羊圈沟为例. 地理学报, 1999, 54(3): 241-246.]

[7] Chen Liding, Fu Bojie, Ingmar Messing. Sustainable land-use planning in a typical catchment in the Loess Plateau: a case study. Geographical Research, 2001, 20(6): 713-722.
[陈利顶, 傅伯杰, Ingmar Messing. 黄土丘陵沟壑区典型小流域土地持续利用案例研究. 地理研究, 2001, 20(6): 713-722.]

[8] Xu Yong, Tian Junliang, Shen Hongquan. Eco-environmental rehabilitation and spatial differentiation based on enlarging terrace and defarming in the Loess Hilly-gully Region. Journal of Natural Resources, 2002, 17(4): 430-437.
[徐勇, 田均良, 沈洪泉. 黄土丘陵区"梯田退耕"生态重建及地域分异特征. 自然资源学报, 2002, 17(4): 430-437.]

[9] Tang Keli, Zhang Keli, Lei Alin. Critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau. Chinese Science Bulletin, 1998, 43(2): 200-203.
[唐克丽, 张科利, 雷阿林. 黄土丘陵区退耕上限坡度的研究论证. 科学通报, 1998, 43(2): 200-203.]

[10] Tian Junliang, Liu Puling, Zhang Yi. The management of soil and water loss to rebuild a graceful Yan'an with green mountains and clean water rivers: understanding and thinking concerning premier Zhu's instructions on eco-environment construction. Research of Soil and Water Conservation, 2000, 7(2): 4-9.
[田均良, 刘普灵, 张翼. 治理水土流失再造山川秀美延安-对中尺度生态环境建设中落实朱总理指示的认识和思考. 水土保持研究, 2000, 7(2): 4-9.]

[11] Peng Wenying, Zhang Keli, Li Shuangcai. Studies of the regional classification about returning farmland to forests or grassland on the Loess Plateau. Journal of Natural Resources, 2002, 17(4): 438-443.
[彭文英, 张科利, 李双才. 黄土高原退耕还林(草)紧迫性地域分级论证. 自然资源学报, 2002, 17(4): 438-443.]

[12] Xu Jiongxin. A study on the coupling relation between the water and sediment yield sub-system and river channel deposition sub-system: an example from the Yellow River. Acta Geographica Sinica, 1997, 52(5):421-429.
[许炯心. 黄河上中游产水产沙系统与下游河道沉积的耦合关系. 地理学报, 1997,52(5):421-429.]

[13] Cai Qiangguo, Shiu-hung Luk, Wang Guiping et al. Process-based soil erosion and sediment yield model in a small basin in the hilly loess region. Acta Geographica Sinica, 1996, 51(2): 108-117.
[蔡强国, 陆兆熊, 王贵平 等. 黄土丘陵沟壑区典型小流域侵蚀产沙过程模型. 地理学报, 1996, 51(2): 108-117.]

[14] Xu Yong. Discussion on the investment problem of rural industrial development based on soil and water conservation. Research of Soil and Water Conservation, 2001, 8(2): 143-146.
[徐勇. 水土保持型农村产业开发投资问题探讨. 水土保持研究, 2001, 8(2): 143-146.]

[15] Jiang Dingsheng, Gao Kexing. Resources potentiality of dam land and pattern of constructing dam system in loess hill region of second section. Bulletin of Soil and Water Conservation, 2000, 20(5): 35-38.
[蒋定生, 高可兴. 黄土丘陵第Ⅱ副区坝地资源潜力与坝系建造模式. 水土保持通报, 2000, 20(5): 35-38.]

[16] Hou Xilu, Cao Qingyu. Study on the benefits of plants to reduce sediment in the loess rolling gullied region of north Shaanxi. Bulletin of Soil and Water Conservation, 1990, 10(2): 19-25.
[侯喜禄, 曹清玉. 陕北黄土丘陵沟壑区植被减沙效益研究. 水土保持通报, 1990, 10(2): 19-25.]

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