岷江上游干旱河谷景观边界动态及其影响域

Dynamics and influence width of dry valley landscape boundary in upper reaches of Minjiang River

采用遥感和地理信息系统技术,界定了岷江上游干旱河谷的范围,在此基础上分析了岷江上游干旱河谷的边界动态及其影响域.结果表明,岷江上游干旱河谷的范围不断扩大,干旱河谷边界长度增加,边界形状复杂性先增加后降低.岷江上游干旱河谷的边界沿山体迅速向上攀升,1974其最高上限为海拔3128m,1995年为3167m,较1974年抬升了39m;2000年为3181m,比1995年抬升了14m.1974—2000年间岷江上游干旱河谷边界最高上限沿垂直方向向上抬升了53m,平均每年约抬升2m.岷江上游干旱河谷边界的显著影响距离为800m,800～1200m为干旱河谷和周围其它景观影响的过渡区域.干旱河谷外缘800m范围内的区域,是干旱河谷抵抗周围景观影响和外来干扰的缓冲地带,在对岷江上游干旱河谷生态环境进行综合治理的过程中,应对其给与充分关注.

Based on RS and GIS techniques, the distribution extent of the dry valley in upper reaches of Minjiang River was determined, with the dynamics and influence width of its landscape boundary analyzed. The results indicated that the dry valley had a gradually expanded distribution, and the total length of its boundary was increased. The boundary complexity increased from 1974 to 1995 but decreased from 1995 to 2000, and the upper boundary of the dry valley ascended rapidly along mountain slope. The uppermost elevation of the dry valley boundary was 3 128 m in 1974, 3 167 m in 1995, and 3 181 m in 2000. In the last 26 years, the upper boundary of the dry valley ascended 53 m in total, being about 2 m per year. The influence width of the dry valley boundary was 800 m, which could be regarded as a buffer zone to disturbances. The area between 800-1200 m from the dry valley boundary to exterior was a transition zone intensely influenced by the dry valley and its surrounding landscape, which should be addressed in the restoration of the dry valley.