مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

video

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

sound

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Version

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

View:

778
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Download:

0
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Cites:

Information Journal Paper

Title

SCALING WATER RETENTION CURVES OF DISSIMILAR SOILS

Pages

  113-120

Abstract

 Scaling methods have been developed to describe the spatial variability of soils. Among them, physically based methods are more desirable in which the scaling factors can be estimated from the soil physical properties. Assuming that the pore size distribution of soils is lognormally distributed, KOSUGI AND HOPMANS developed a physically based method to scale the water retention curve. However, similar to the previous methods, application of this method is limited to the similar soils. To alleviate this limitation, in this paper, a physically based method is proposed for DISSIMILAR SOILS. Using this method, data of a wide textural range of soils can be scaled without the similarity condition and can be represented by a unique EXPONENTIAL REFERENCE CURVE. This method was validated using 487 sets of soil retention curves taken from UNSODA database including all the textural classes from sand to clay. The results showed that the proposed method had a better performance in scaling the retention curves than that of KOSUGI AND HOPMANS. The criteria defined here for scaling error was obtained equal to 0.074 and 0.105 for the proposed and Kosugi-Hopmans method, respectively. In addition, it was shown that, in contrast to the previous methods, the scaling error of the proposed method does not depend on the soil texture and all the soils have an equal chance for being scaled.

Cites

  • No record.
  • References

    Cite

    APA: Copy

    GHAHRAMAN, B., SADEGHI, M., & GOHAR DOUST MONFARED, M.R.. (2012). SCALING WATER RETENTION CURVES OF DISSIMILAR SOILS. IRANIAN WATER RESEARCH JOURNAL, 5(9), 113-120. SID. https://sid.ir/paper/159747/en

    Vancouver: Copy

    GHAHRAMAN B., SADEGHI M., GOHAR DOUST MONFARED M.R.. SCALING WATER RETENTION CURVES OF DISSIMILAR SOILS. IRANIAN WATER RESEARCH JOURNAL[Internet]. 2012;5(9):113-120. Available from: https://sid.ir/paper/159747/en

    IEEE: Copy

    B. GHAHRAMAN, M. SADEGHI, and M.R. GOHAR DOUST MONFARED, “SCALING WATER RETENTION CURVES OF DISSIMILAR SOILS,” IRANIAN WATER RESEARCH JOURNAL, vol. 5, no. 9, pp. 113–120, 2012, [Online]. Available: https://sid.ir/paper/159747/en

    Related Journal Papers

    Related Seminar Papers

  • No record.
  • Related Plans

  • No record.
  • Recommended Workshops






    Move to top
    telegram sharing button
    whatsapp sharing button
    linkedin sharing button
    twitter sharing button
    email sharing button
    email sharing button
    email sharing button
    sharethis sharing button