摘要
利用航空影像分析黄土丘陵沟壑区周屯沟小流域(面积33.6km2)瓦背状浅沟分布规律。浅沟主要发育在坡耕地上。流域内,浅沟分布区占坡面面积的31.3%,集中分布,平均频数7.2条/100m横坡面,密度为4~9条/100m的浅沟坡面占78%。相关分析表明,浅沟频数与浅沟的长度、浅沟坡面的总坡度显著相关。浅沟的平均长度64.7m,30~110m长的浅沟占91%,浅沟坡面总平均坡度数23°,13~32°的占95%。瓦背状浅沟实质上是坡耕地上一种产沙量较高的稳定地貌形态。
The distribution of shallow gully of Zhondunguo watershed in the loess hilly and gully regions were showed using the results from WB aerial photograph interpretation. The shallow gully covers 31.3% of total areas of hillslope in the watershed. It is average frequency(density) 7.2/100 m cross section of hillslope , the frequency range 49/100 m accounts for 78%. The total average degree of shallow gully hillside is 23;range 1232 is 95%. It is average length 67.4 m, range 30110 m is 91%. In fact, tileroofed shape shallow gully is a more stable geographical feature which can yield a higher silt. Interrelation analysis reveals a significant relationship between shallow gully density and total hillslope degree or shallow gully length.
出处
《水土保持研究》
CSCD
1999年第2期181-184,共4页
Research of Soil and Water Conservation
基金
陕西省自然科学基金
关键词
瓦背状
浅沟
坡面
土壤侵蚀
斜坡
shallow gullyhillslope processessoil erosion T