Runoff and soil loss from bench terraces. 1. An event-based model of rainfall infiltration and surface runoff.

A.I.J.M. van Dijk; L.A. Bruijnzeel

doi:10.1111/j.1365-2389.2004.00604.x

Runoff and soil loss from bench terraces. 1. An event-based model of rainfall infiltration and surface runoff.

A.I.J.M. van Dijk, L.A. Bruijnzeel

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Overland flow resulting from an excess of rain over infiltration is an essential component of many models of runoff and erosion from fields or catchments. The spatially variable infiltration (SVI) model and a set of associated equations relating depth of runoff and maximum rate of 'effective' runoff (as used in the GUEST erosion model) to storm depth, depth-averaged intensity of rainfall, average maximum infiltration capacity and an additional amount of initial infiltration were validated and tested on back-sloping bench terraces in volcanic upland West Java, Indonesia. Data used were runoff rate and depth from 31 small (1.0-8.2 m

Original language	English
Pages (from-to)	299-316
Journal	European Journal of Soil Science
Volume	55
DOIs	https://doi.org/10.1111/j.1365-2389.2004.00604.x
Publication status	Published - 2004

Access to Document

10.1111/j.1365-2389.2004.00604.x

Handle.net

Persistent link

Cite this

@article{549adb911b50486984136ce4c40a5e2d,

title = "Runoff and soil loss from bench terraces. 1. An event-based model of rainfall infiltration and surface runoff.",

abstract = "Overland flow resulting from an excess of rain over infiltration is an essential component of many models of runoff and erosion from fields or catchments. The spatially variable infiltration (SVI) model and a set of associated equations relating depth of runoff and maximum rate of 'effective' runoff (as used in the GUEST erosion model) to storm depth, depth-averaged intensity of rainfall, average maximum infiltration capacity and an additional amount of initial infiltration were validated and tested on back-sloping bench terraces in volcanic upland West Java, Indonesia. Data used were runoff rate and depth from 31 small (1.0-8.2 m",

author = "{van Dijk}, A.I.J.M. and L.A. Bruijnzeel",

year = "2004",

doi = "10.1111/j.1365-2389.2004.00604.x",

language = "English",

volume = "55",

pages = "299--316",

journal = "European Journal of Soil Science",

issn = "1351-0754",

publisher = "Wiley-Blackwell",

}

TY - JOUR

T1 - Runoff and soil loss from bench terraces. 1. An event-based model of rainfall infiltration and surface runoff.

AU - van Dijk, A.I.J.M.

AU - Bruijnzeel, L.A.

PY - 2004

Y1 - 2004

N2 - Overland flow resulting from an excess of rain over infiltration is an essential component of many models of runoff and erosion from fields or catchments. The spatially variable infiltration (SVI) model and a set of associated equations relating depth of runoff and maximum rate of 'effective' runoff (as used in the GUEST erosion model) to storm depth, depth-averaged intensity of rainfall, average maximum infiltration capacity and an additional amount of initial infiltration were validated and tested on back-sloping bench terraces in volcanic upland West Java, Indonesia. Data used were runoff rate and depth from 31 small (1.0-8.2 m

AB - Overland flow resulting from an excess of rain over infiltration is an essential component of many models of runoff and erosion from fields or catchments. The spatially variable infiltration (SVI) model and a set of associated equations relating depth of runoff and maximum rate of 'effective' runoff (as used in the GUEST erosion model) to storm depth, depth-averaged intensity of rainfall, average maximum infiltration capacity and an additional amount of initial infiltration were validated and tested on back-sloping bench terraces in volcanic upland West Java, Indonesia. Data used were runoff rate and depth from 31 small (1.0-8.2 m

U2 - 10.1111/j.1365-2389.2004.00604.x

DO - 10.1111/j.1365-2389.2004.00604.x

M3 - Article

SN - 1351-0754

VL - 55

SP - 299

EP - 316

JO - European Journal of Soil Science

JF - European Journal of Soil Science

ER -

Runoff and soil loss from bench terraces. 1. An event-based model of rainfall infiltration and surface runoff.

Abstract

Access to Document

Handle.net

Fingerprint

Cite this