地球信息科学学报 ›› 2017, Vol. 19 ›› Issue (3): 355-364.doi: 10.3724/SP.J.1047.2017.00355
杜国明1,2(), 孙晓兵1, 刘彦随2, 郑惠玉1, 马榕徽1
收稿日期:
2016-03-28
修回日期:
2016-05-23
出版日期:
2017-03-20
发布日期:
2017-03-20
作者简介:
作者简介:杜国明(1978-),男,博士,教授,研究方向为土地资源优化配置。E-mail:
基金资助:
DU Guoming1,2,*(), SUN Xiaobing1, LIU Yansui2, ZHENG Huiyu1, MA Ronghui1
Received:
2016-03-28
Revised:
2016-05-23
Online:
2017-03-20
Published:
2017-03-20
Contact:
DU Guoming
摘要:
生态退耕是调整陆地生态系统结构与功能以应对土地利用过度干扰的重要途径之一,因此科学掌握退耕格局与耕地格局演变对黄土高原生态环境治理与生态修复具有深远意义。本文以位于黄土高原的延安市为典型区,从生态退耕的整体特征、地形因素及区域差异等角度,探究生态退耕以来其耕地变化及退耕状况的空间分异特征。结果表明:生态退耕致使延安市耕地面积由2000年的11 752.80 km2减少为2013年的9149.93 km2,退耕面积为2756.85 km2,退耕指数为22.15%,且退耕耕地主要转化为林地、草地,占退耕面积的95.29%;耕地与退耕面积主要分布于6~15°、15~25°坡度及第II级(925~1115 m)、第III级(1115~1275 m),且2005-2013年的生态退耕速率均高于2000-2005年的生态退耕速率;县域退耕面积及退耕程度均呈现由北向南依次递减的分异特征,而退耕重心与耕地重心均在延安市几何中心以北的安塞县与宝塔区边界,且生态退耕的重心由东北向西南方向迁移,耕地重心则由北向南迁移。本文通过对延安市生态退耕的时空分异特征分析可为黄土高原更加科学合理地推进生态保育与生态文明建设提供参考。
杜国明, 孙晓兵, 刘彦随, 郑惠玉, 马榕徽. 黄土高原生态退耕的时空分异特征[J]. 地球信息科学学报, 2017, 19(3): 355-364.DOI:10.3724/SP.J.1047.2017.00355
DU Guoming,SUN Xiaobing,LIU Yansui,ZHENG Huiyu,MA Ronghui. Temporal and Spatial-Differentiation Characteristics of Ecological Restoration in Loess Plateau[J]. Journal of Geo-information Science, 2017, 19(3): 355-364.DOI:10.3724/SP.J.1047.2017.00355
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