2001
DOI: 10.1097/00010694-200107000-00002
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Soil Degradation Related to Overgrazing in the Semi-Arid Southern Caldenal Area of Argentina

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Cited by 63 publications
(33 citation statements)
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“…Soil recovery may have to occur first because increased soil penetration resistance and decreased aggregate stability can reduce the amount of water available for plant growth (Boxell and Drohan 2009). In addition, high soil penetration resistance can restrict root growth (Ehlers et al 1983, Bengough and Mullin 1991, Villamil et al 2001. Soil compaction and trampling by large herbivores can also inhibit plant diversity (Olff and Ritchie 1998).…”
Section: Discussionmentioning
confidence: 99%
“…Soil recovery may have to occur first because increased soil penetration resistance and decreased aggregate stability can reduce the amount of water available for plant growth (Boxell and Drohan 2009). In addition, high soil penetration resistance can restrict root growth (Ehlers et al 1983, Bengough and Mullin 1991, Villamil et al 2001. Soil compaction and trampling by large herbivores can also inhibit plant diversity (Olff and Ritchie 1998).…”
Section: Discussionmentioning
confidence: 99%
“…In some places, these lacustrine sediments are superimposed by layers of coarse-textured material deriving from eolian sediments or colluvial deposits, thus increasing the vertical heterogeneity of the soil texture. The economic activities of the local population have had a detrimental effect on soil quality, and the surface horizons of soils where over grazing has occurred, have a marked structural deterioration compared with ungrazed soils (Villamil et al, 2001).…”
Section: Soilsmentioning
confidence: 99%
“…The Caldenal region included in the rangeland area of Argentina occupies about 40,000 km 2 between approximately 32° and 40°S latitude. The region is a transition between the Monte desert to the west and the cultivated humid Pampa to the east.…”
Section: Introductionmentioning
confidence: 99%
“…Total porosity in the top few centimeters are lower in grazed than in ungrazed areas (17%) due to the collapse of large pores. There is a marked reduction in the quantity and density of roots in the top soil horizon and there are also changes in the mean diameter of roots [2].…”
Section: Introductionmentioning
confidence: 99%