Research on control way for cultivated land in karst rocky desertification basin—A case in Shiqiao Basin, Bijie City and Mugong Basin, Guanling City in Guizhou Province
-
摘要: 贵州毕节石桥小流域与关岭木工小流域处于石漠化严重、坡耕地比例高、粮食产量低且不稳定、人口密度大、农业经济水平低的喀斯特山区。通过对研究区人口增长的预测,利用人-地关系平衡模型,计算出该两小流域需保有的耕地量分别为281.91hm2、228.68hm2。但由于需保有的耕地面积较未出现石漠化耕地面积大,致使需保有的耕地中仍有部分地存在石漠化。但如果对这部分石漠化土地都实施退耕还林还草,将无法保障流域内农民的口粮需求。为此,对该两小流域耕地石漠化区域开展包括林农间作、粮草间作、坡改梯等治理措施。结果流域内耕地的石漠化得到了有效控制,土壤侵蚀模数由2007年的721.63t/(km2?a)、42.42t/(km2?a)下降到2009年的472.78t/(km2?a)、35.59t/(km2?a),植被覆盖率分别提高11.3%、6.4%,人均经济收入分别增加300元和231元,不仅有效地治理了石漠化耕地,而且农民生计也得到了保障。Abstract: Shiqiao Basin in Bijie City and Mugong Basin in Guanling City in Guizhou Province are karst rocky mountain areas with strong rocky desertification, high density of population, and low and instable grain yield as well as low agricultural economic level. Through forecasting the increase trend of the population and using the human-land balance model, the necessary farmlands for these two basins have been counted as 281.91 hm2 and 228.68 hm2, However, the area of necessary farmland is larger than non-desertification farm-land, which leads to rocky desertification still appear in the farmland. If the grain for green project has been carried out in this place, it will not meet the need for food. Therefore, the measures as intercropping of trees and crops, crop-grass intercropping, reforming sloping fields to terraced fields have been carried out. As a result, rocky desertification has been controlled and soil erosion modulus of the two basins has decreased from 721.63t/(km2?a) and 42.42t/(km2?a) in 2007 to 472.78t/(km2?a) and 35.59t/(km2?a) in 2009, vegetation covered lands have increased by 11.3% and 6.4%, per capital income has increased by 300 Yuan and 231 Yuan. Rocky desertification has been controlled as well as peasants have got much more livelihood safety.
-
[1] 陈奇伟,熊康宁,蓝安军.基于“3S”的贵州喀斯特石漠化现状及变化趋势分析[J].中国岩溶,2007,26(1):37-42. [2] 熊康宁,盈斌,罗娅,等.喀斯特石漠化的演变趋势与综合治理[J].世界林业研究,2009,22(特刊):18-23. [3] 刘拓,周光辉,但新球,等.中国岩溶石漠化——现状、成因与防治[M].北京:中国林业出版社,2009:1-12. [4] 许静.石漠化年吞噬贵州耕地30万亩[EB].http://www.chi-na.com.cn/tech/zhuanti/wyh/2008-01/16/content_9539353.htm,2005-6-17/2010-4-03. [5] 熊康宁,黎平,周忠发,等.喀斯特石漠化的遥感-GIS典型研究——以贵州省为例[M].北京:地质出版社,2002:42-44. [6] 谢高地,成升魁,丁贤忠.人口增长胁迫下的全球土地利用变化研究[J].自然资源学报,1999,14(3):193-199. [7] 杨明德.喀斯特流域结构特性及其水文效益[C]//杨明德.喀斯特研究——杨明德论文集.贵阳:贵州民族出版社,2003:127-136. [8] 李阳兵,王世杰,李瑞玲,等.花江喀斯特峡谷地区石漠化成因初探[J].水文地质工程地质,2004,(6):37-42. [9] 苏维词,杨华.典型喀斯特峡谷石漠化地区生态农业模式探析——以贵州省花江大峡谷顶坛片区为例[J].中国生态农业学报,2005,13(4):218-220. [10] 容丽,熊康宁.花江喀斯特峡谷适生植物的抗旱特征Ⅰ:顶坛花椒根系与土壤环境[J].贵州师范大学学报(自然科学版),2007,25(4):1-7,34. [11] 苏孝良,于东平,高武国.喀斯特石漠化地区种植金银花的生态与经济效益[J].贵州林业科技,2005,33(1):50-54. -

计量
- 文章访问数: 2011
- HTML浏览量: 421
- PDF下载量: 1607
- 被引次数: 0