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Recovery of soil phosphorus on former bauxite mines through tropical forest restoration
Author(s) -
Bizuti Denise T. G.,
Marchi Soares Thaís,
Duarte Marina M.,
Casagrande José C.,
Souza Moreno Vanessa,
Peinado Francisco J. M.,
Sartorio de Medeiros Simone D.,
Melis Juliano,
Schweizer Daniella,
Brancalion Pedro H. S.
Publication year - 2020
Publication title -
restoration ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.214
H-Index - 100
eISSN - 1526-100X
pISSN - 1061-2971
DOI - 10.1111/rec.13194
Subject(s) - topsoil , bauxite , phosphorus , nutrient , environmental science , restoration ecology , soil water , forest restoration , organic matter , agronomy , environmental chemistry , chemistry , forest ecology , ecology , soil science , biology , ecosystem , organic chemistry
Soil phosphorus (P) is a major driver of forest development and a critically limited nutrient in tropical soils, especially when topsoil is removed by mining. This nutrient can be present in soils in the form of different fractions, which have direct consequences for P availability to plants and, consequently, for restoration success. Therefore, understanding how the stocks of different soil P fractions change over the restoration process can be essential for guiding restoration interventions, monitoring, and adaptive management. Here, we investigated the recovery of soil P fractions by forest restoration interventions on bauxite mine sites in the Brazilian Atlantic Forest. We assessed the concentration of different fractions of soil organic and inorganic P at (1) a bauxite mine prepared for restoration; (2) two former bauxite mines undergoing forest restoration for 6 and 24 years; and (3) an old‐growth forest remnant. Overall, restored areas recovered levels of labile organic P (P o ‐NaHCO 3 ) at 5–40 cm and of moderately labile organic P (P o ‐NaOH) at different depths, exhibiting concentrations similar to those found in a conserved forest. The use of P‐rich fertilizers and forest topsoil may have greatly contributed to this outcome. Some other fractions, however, recovered only after 24 years of restoration. Other inorganic P fractions did not differ among mined, restored, and conserved sites: nonlabile P i (residual P and P‐HCl), labile P i (P i ‐NaHCO 3 ), and moderately labile P i (P i ‐NaOH). Forest restoration was able to promote efficient recovery of important soil P fractions, highlighting the value of restoration efforts to mitigate soil degradation by mining.