Effects of livestock grazing on physical and chemical properties of sandy soils in Sahelian rangelands

Citation
P. Hiernaux et al., Effects of livestock grazing on physical and chemical properties of sandy soils in Sahelian rangelands, J ARID ENV, 41(3), 1999, pp. 231-245
Citations number
48
Categorie Soggetti
Environment/Ecology
Journal title
JOURNAL OF ARID ENVIRONMENTS
ISSN journal
01401963 → ACNP
Volume
41
Issue
3
Year of publication
1999
Pages
231 - 245
Database
ISI
SICI code
0140-1963(199903)41:3<231:EOLGOP>2.0.ZU;2-3
Abstract
The effects of grazing by livestock on soil surface features, bulk density and chemical properties were studied at the completion of a 4-year grazing experiment carried out in Sadore, Niger. Grazing treatments were a factoria l arrangement of two stocking rates (62.5 and 125 kg live weight ha(-1)) an d four sheep:goat ratios (0:6, 2:4, 4:2 and 6:0 animals per pasture), with two pastures per treatment and two ungrazed controls. Observations were als o made in a fallow subjected to 9 years of intense and uncontrolled mixed g razing, and in a site that had been protected from grazing for 15 years. Th e topsoil was sampled (at depths of 0-2, 2-6, 6-14 and 14-30 cm) below shru b canopy in herbaceous vegetation and in bare soil patches within each of 2 0 paddocks for determination of pH, organic C, and total N and P concentrat ions. Soil bulk density was measured in a subset of soil profiles. The area l extent of different types of soil crusts and other soil surface features was assessed in one-half of the paddocks. Grazing resulted in a reduction ( p < 0.01) and fragmentation of the area of crusted soils. However, this tre nd was partially compensated for by an increase of newly formed crusts. As a result, the soil infiltration index slightly increased with moderate graz ing, but decreased at higher stocking rates. Compaction due to trampling wa s observed ih the topsoil beneath the shrub canopy and also in vegetated pa tches, but only under intense grazing pressure. Soil bulk density was not a ffected by grazing except for an increase observed below 10 cm depth at the understorey of shrubs which is therefore unlikely due to trampling. When c ompared to the ungrazed control, pH, organic C and N concentrations, and to lesser extent P concentration, decreased after 4 years of grazing. Soil P and pH further decreased after 9 years of very high grazing pressure. Howev er, neither N nor organic C decreased further. (C) 1999 Academic Press.