Agricultural watershed modeling: a review for hydrology and soil erosion processes

被引:41
作者
de Mello, Carlos Rogerio [1 ]
Norton, Lloyd Darrell [2 ]
Pinto, Leandro Campos [3 ]
Beskow, Samuel [3 ]
Curi, Nilton [4 ]
机构
[1] Univ Fed Lavras UFLA, Dept Engn DEG, Lavras, MG, Brazil
[2] Purdue Univ, USDA ARS, Natl Soil Eros Res Lab, W Lafayette, IN 47907 USA
[3] Univ Fed Pelotas UFPel, Pelotas, RS, Brazil
[4] Univ Fed Lavras UFLA, Dept Ciencia Solo, Lavras, MG, Brazil
来源
CIENCIA E AGROTECNOLOGIA | 2016年 / 40卷 / 01期
关键词
RUSLE; WEPP; GeoWEPP; LASH; DHSVM; AnnAGNPS; SOURCE POLLUTION MODEL; GRANDE RIVER-BASIN; PROJECT WEPP MODEL; LAND-USE CHANGES; ANNAGNPS MODEL; SEDIMENT YIELD; CLIMATE-CHANGE; SWAT MODEL; VEGETATION MODEL; RUNOFF;
D O I
10.1590/S1413-70542016000100001
中图分类号
S [农业科学];
学科分类号
09 ;
摘要
Models have been used by man for thousands of years to control his environment in a favorable way to better human living conditions. The use of hydrologic models has been a widely effective tool in order to support decision makers dealing with watersheds related to several economic and social activities, like public water supply, energy generation, and water availability for agriculture, among others. The purpose of this review is to briefly discuss some models on soil and water movement on landscapes (RUSLE, WEPP, GeoWEPP, LASH, DHSVM and AnnAGNPS) to provide information about them to help and serve in a proper manner in order to discuss particular problems related to hydrology and soil erosion processes. Models have been changed and evaluated significantly in recent years, highlighting the use of remote sense, GIS and automatic calibration process, allowing them capable of simulating watersheds under a given land-use and climate change effects. However, hydrology models have almost the same physical structure, which is not enough for simulating problems related to the long-term effects of different land-uses. That has been our challenge for next future: to understand entirely the hydrology cycle, having as reference the critical zone, in which the hydrological processes act together from canopy to the bottom of aquifers.
引用
收藏
页码:7 / 25
页数:19
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