The ultimately stable slopes in the cases of seepage through the earth dam, under the sheet piling, and to the drainage trench are founded by the methods of linear differential equations, boundary-value problems, and hodograph of velocity.

  • INTRODUCTION

  • 1, A STABLE SLOPE OF AN EARTH DAM

  • 2. A STABLE BOUNDARY OF A DOWNSTREAM SLOPE

  • 3. A STABLE PROFILE OF A DRAINAGE TRENCH

  • RESULTS

  • REFERENCES

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