Aiming at alleviating the serious soil erosion, the Chinese government initiated the Sloping Land Conversion Program (SLCP) in 1999. Now, after 8 years of project implementation, the ecological recovery effects of the...Aiming at alleviating the serious soil erosion, the Chinese government initiated the Sloping Land Conversion Program (SLCP) in 1999. Now, after 8 years of project implementation, the ecological recovery effects of the SLCP have become the hot issue of academic circle. This paper, taking the loess hill and gully area of northern Shaanxi as an example, presents a methodology for assessing the vegetation restoration effect of SLCP with normalized difference vegetation index (NDVI). The key components include calculation of the Growing Season NDVI (GSNDVI), and estimation of the NVDI change induced by climate and SLCP, respectively. Based on the method, the NDVI change between 2000 and 2006 was obtained using the GSNDVI that excluded the noise from snow and ice. After the part of total NDVI change caused by climate variation was estimated using empiric formulae, we obtained the part induced by human factors, i.e. the SLCP. The human induced part of NDVI change was considered as an approximation indicating the effect of the SLCP on the vegetation. Finally, we analyzed the NDVI change characters of the whole study area, different slope lands and different land use types by spatial statistics method. Results show that the vegetation condition is significantly improved by the SLCP, particularly land types that directly involved in the SLCP, such as steeply slope farmlands, degraded grasslands, etc.展开更多
Dae to complex terrain of the Loess Plateau, the classification accuracy is unsatisfactory when a single supervised classification is used in die remote sensing investigation of the sloping field. Taking the loess hil...Dae to complex terrain of the Loess Plateau, the classification accuracy is unsatisfactory when a single supervised classification is used in die remote sensing investigation of the sloping field. Taking the loess hill and gully area of northern Shaanxi Province as a test area, a research was conducted to extract sloping field and other land use categories by applying an integrated classification. Based on an integration of supervised classification aad unsupervised classification, sampling method is remarkably unproved. The results show that the classification accuracy is satisfactory by the method and is of critical significance in obtaining up-to-date information of the sloping field, which should be helpful in the state key project of converting farmland to forest and grassland on slope land in this area. This research sought to improve the application accuracy of image classification in complex terrain areas.展开更多
关中唐十八帝陵是古代中国留给后代宝贵的历史文化遗产,千年以来帝陵遗址区水土流失现象加剧,破坏了帝陵景观。为了保护文化遗产,本文以某唐帝陵为对象,使用卫星和无人机影像产品,估算53年来司马道冲沟的发育速率,建立了帝陵遗址区的水...关中唐十八帝陵是古代中国留给后代宝贵的历史文化遗产,千年以来帝陵遗址区水土流失现象加剧,破坏了帝陵景观。为了保护文化遗产,本文以某唐帝陵为对象,使用卫星和无人机影像产品,估算53年来司马道冲沟的发育速率,建立了帝陵遗址区的水土流失体积-面积关系模型。结果表明:①遗址区受益于还林换草工程,坡耕地减少,草地林地增加。司马道下游林区NDVI指数达0.8,生态环境明显好转,水土流失等级转为轻度。②渭北旱塬地区,发育为卵状冲沟与其垂直面的切沟,周长与面积有良好的拟合关系。③唐帝陵遗址区的沟道发育模型,面积和体积之间有良好的幂函关系,即y=0.0405 x 1.4936,决定系数R 2=0.82,53年来的切沟年发育为0.36 m/a。可将上述模型作为渭北旱塬地区沟道发育模型。④遗址区水土流失和土壤沉积体积比率为38.5∶1,产生的侵蚀和土壤沉积面积比率为11.5∶1。展开更多
基金supported by National Natural Science Foundation of China (Grant No.40671007) Major Projects of Knowledge In-novation Program of the Chinese Academy of Sciences (Grant No.KZCX2-YW-421)
文摘Aiming at alleviating the serious soil erosion, the Chinese government initiated the Sloping Land Conversion Program (SLCP) in 1999. Now, after 8 years of project implementation, the ecological recovery effects of the SLCP have become the hot issue of academic circle. This paper, taking the loess hill and gully area of northern Shaanxi as an example, presents a methodology for assessing the vegetation restoration effect of SLCP with normalized difference vegetation index (NDVI). The key components include calculation of the Growing Season NDVI (GSNDVI), and estimation of the NVDI change induced by climate and SLCP, respectively. Based on the method, the NDVI change between 2000 and 2006 was obtained using the GSNDVI that excluded the noise from snow and ice. After the part of total NDVI change caused by climate variation was estimated using empiric formulae, we obtained the part induced by human factors, i.e. the SLCP. The human induced part of NDVI change was considered as an approximation indicating the effect of the SLCP on the vegetation. Finally, we analyzed the NDVI change characters of the whole study area, different slope lands and different land use types by spatial statistics method. Results show that the vegetation condition is significantly improved by the SLCP, particularly land types that directly involved in the SLCP, such as steeply slope farmlands, degraded grasslands, etc.
基金National Nature Science Foundation of China,No.40271089High-visiting scholar fund of The Key Laboratory of LIESMARS
文摘Dae to complex terrain of the Loess Plateau, the classification accuracy is unsatisfactory when a single supervised classification is used in die remote sensing investigation of the sloping field. Taking the loess hill and gully area of northern Shaanxi Province as a test area, a research was conducted to extract sloping field and other land use categories by applying an integrated classification. Based on an integration of supervised classification aad unsupervised classification, sampling method is remarkably unproved. The results show that the classification accuracy is satisfactory by the method and is of critical significance in obtaining up-to-date information of the sloping field, which should be helpful in the state key project of converting farmland to forest and grassland on slope land in this area. This research sought to improve the application accuracy of image classification in complex terrain areas.
文摘关中唐十八帝陵是古代中国留给后代宝贵的历史文化遗产,千年以来帝陵遗址区水土流失现象加剧,破坏了帝陵景观。为了保护文化遗产,本文以某唐帝陵为对象,使用卫星和无人机影像产品,估算53年来司马道冲沟的发育速率,建立了帝陵遗址区的水土流失体积-面积关系模型。结果表明:①遗址区受益于还林换草工程,坡耕地减少,草地林地增加。司马道下游林区NDVI指数达0.8,生态环境明显好转,水土流失等级转为轻度。②渭北旱塬地区,发育为卵状冲沟与其垂直面的切沟,周长与面积有良好的拟合关系。③唐帝陵遗址区的沟道发育模型,面积和体积之间有良好的幂函关系,即y=0.0405 x 1.4936,决定系数R 2=0.82,53年来的切沟年发育为0.36 m/a。可将上述模型作为渭北旱塬地区沟道发育模型。④遗址区水土流失和土壤沉积体积比率为38.5∶1,产生的侵蚀和土壤沉积面积比率为11.5∶1。
