Earticle

초록

영어

The relationship between hydrologic processes and scale is one of the more complex issues in surface water hydrology. Disturbances that change vegetation and/or soil properties have been known to subsequently alter the landscape. The primary objective of this study was to estimate the grain size of soils with different properties from the hydraulic conductivity using pedotransfer functions. The double ring infiltrometer method was used to measure the vertical hydraulic conductivity of three soils under different soil planar surface treatments. Seven selected pedotransfer functions were used to estimate percentile diameters and the reduction in infiltration caused by compaction was misconstrued as caused by changes in percentile diameter. Results showed that compaction on the sandy loamy foot paths reduced the hydraulic conductivity by about 50%. The study showed that perceptual models of infiltration processes and appreciation of scale problems in modeling are far more sophisticated than normally presented in texts. Hydraulic measurement methods are still relevant and will provide significant information of grain size of the soils.

키워드

저자

• 은코모제피 템바 [ Nkomozepi, Temba | Department of Agricultural Engineering, Kyungpook National University ]
• 정상옥 [ Chung, Sang-Ok | Department of Agricultural Engineering, Kyungpook National University ]

참고문헌

발행기관

간행물

표지보기 관심저널 등록

• 간행물명

  경북대농학지

• 간기

  계간

• pISSN

  2287-271X

• eISSN

  2288-0356

• 수록기간

  ~2014

• 십진분류

  KDC 525 DDC 635