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. 2013 Jun 5;368(1619):20120154. doi: 10.1098/rstb.2012.0154

Table 2.

Phosphorus (P) sorption isotherm variables (Smax, KL and r2) based on the Langmuir equation calculated for each land use (forest and soya bean fields converted to soya bean in 2003, 2004, 2007 and 2008). Soil samples were taken in January and February 2009 at Tanguro Ranch in Mato Grosso, Brazil. Langmuir equations for each land use were based on the data from seven soil cores.

land use depth KL Smax r2
forest 10 0.0281 834 0.9422
20 0.0198 1270 0.9995
50 0.0107 2320 0.9997
soya bean 2003 10 0.0347 728 0.9964
20 0.0186 1340 1.0000
50 0.00485 5120 0.9997
soya bean 2004 10 0.0272 901 0.9988
20 0.0277 904 0.9983
50 0.00784 3190 0.9995
soya bean 2007 10 0.106 239 0.9971
20 0.0975 262 0.9989
50 0.0345 737 0.9998
soya bean 2008 10 0.0342 709 0.9861
20 0.00866 2870 0.9893
50 0.00114 21 800 0.9991
mean 0.026 2640