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Soil Carbon and Nutrient Changes Associated with Deforestation for Pasture in Southern Costa Rica
Author(s) -
Huth Timothy,
Porder Stephen,
Chaves Joaquin,
Whiteside Jessica H.
Publication year - 2012
Publication title -
biotropica
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.813
H-Index - 96
eISSN - 1744-7429
pISSN - 0006-3606
DOI - 10.1111/j.1744-7429.2012.00863.x
Subject(s) - topsoil , pasture , deforestation (computer science) , environmental science , soil carbon , nutrient , agroforestry , phosphorus , erosion , soil retrogression and degradation , agronomy , forestry , soil water , geography , ecology , soil science , biology , chemistry , paleontology , organic chemistry , computer science , programming language
We assessed the effects of deforestation on soil carbon (C) and nutrient stocks in the premontane landscape near Las Cruces Biological Station in southern Costa Rica, where forests were cleared for pasture in the mid‐1960s. We excavated six soil pits to a depth of 1 m in both pasture and primary forest, and found that C stocks were ~20 kg C/m 2 in both settings. Nevertheless, soil δ 13 C suggests ~50 percent of the forest‐derived soil C above 40 cm depth has turned over since deforestation. Soil nitrogen (N) and phosphorus (P) stocks derived from the soil pits were not significantly different between land uses ( P = 0.43 and 0.61, respectively). At a larger spatial scale, however, the ubiquity of ruts produced by cattle‐induced erosion indicates that there are substantial soil effects of grazing in this steep landscape. Ruts averaged 13 cm deep and covered ~45 percent of the landscape, and thus are evidence of the removal of 0.7 Mg C/ha/yr, and 70, 9 and 40 kg/ha/yr of N, P and potassium (K), respectively. Subsoils in this region are ~10 times less C‐ and N‐rich, and ~2 times less P‐ and K‐rich than the topsoil. Thus, rapid topsoil loss may lead to a decline in pasture productivity in the coming decades. These data also suggest that the soil C footprint of deforestation in this landscape may be determined by the fate of soil C as it is transported downstream, rather than C turnover in situ .