水土保持学报
水土保持學報
수토보지학보
JOURNAL OF SOIL AND WATER CONSERVATION
2001年
1期
122-125
,共4页
黄土沟谷%沟谷侵蚀%均衡纵剖面
黃土溝穀%溝穀侵蝕%均衡縱剖麵
황토구곡%구곡침식%균형종부면
均衡纵剖面是一切水道发育的最终形态,其标准形式是摆线。以实际沟谷与标准摆线间的差异为依据,初步建立了由摆线相关度和沟谷纵剖面几何形态参数两类指标构成的沟谷下蚀趋势评价指标体系,并以鸭儿沟为例进行了实际验证,结果较符合实际。
均衡縱剖麵是一切水道髮育的最終形態,其標準形式是襬線。以實際溝穀與標準襬線間的差異為依據,初步建立瞭由襬線相關度和溝穀縱剖麵幾何形態參數兩類指標構成的溝穀下蝕趨勢評價指標體繫,併以鴨兒溝為例進行瞭實際驗證,結果較符閤實際。
균형종부면시일절수도발육적최종형태,기표준형식시파선。이실제구곡여표준파선간적차이위의거,초보건립료유파선상관도화구곡종부면궤하형태삼수량류지표구성적구곡하식추세평개지표체계,병이압인구위례진행료실제험증,결과교부합실제。
The equilibrium profile is the ultimate form of all water course. Its standar form is rotation-wheel-line.Based on the difference between actura l gulley and standar rotation-wheel-line,this paper establishes an assessment system that compose of two types of index, the interrelated degree and sha pe parameter of gulley's profile,to calculate the down-erosion trend of gulley.The results show the evaluating results using index system conform to rea lity while taking Yaer gulley as an example to test this system.