Details

Autor(en) / Beteiligte

• Matus, F.J
• Lusk, C.H
• Maire, C.R

Titel

Effects of Soil Texture, Carbon Input Rates, and Litter Quality on Free Organic Matter and Nitrogen Mineralization in Chilean Rain Forest and Agricultural Soils

Ist Teil von

• Communications in soil science and plant analysis, 2008-01, Vol.39 (1-2), p.187-201

Ort / Verlag

Philadelphia, PA: Taylor & Francis Group

Erscheinungsjahr

2008

Quelle

Taylor & Francis

Beschreibungen/Notizen

• Nitrogen (N) mineralization in soil depends on carbon (C) input of plant materials, site environmental conditions, and soil texture. Empirical correlates of N mineralization can be difficult to interpret, however, because of interactions among these factors. A multiple regression model relating N mineralization to C input rates, litter quality, and soil texture in Chilean temperate rain forest soils was developed. Nitrogen mineralization rates ranged from 3.0 to 5.7 mg kg⁻¹ soil d⁻¹ depending on C input rate and soil texture but were not influenced by litter quality. We compared C storage of both forest and long-term-cropped soils with the protective capacity (i.e., the expected maximum C pool associated with the clay and silt fractions). Soil organic C associated with the fine fraction of forest soils was significantly greater than the calculated protective capacity, with clay-rich soils averaging 141% more C than this limit and coarser soils having 56% more than predicted. In contrast, C content of cropped soils was well below the calculated protective capacity, averaging approximately 32-60% less than this limit, showing the potential of these soils for sequestering C. The results were consistent with the finding that N mineralization was positively correlated with the amount of free organic matter associated with the sand-size fraction in forest soils. The study illustrates that (i) the capacity of soils to preserve soil organic C in clay- and silt-sized particles was greater than that of agricultural soils and (ii) in highly saturated soils, the N mineralization is a function of the quantity of organic-matter input, which in turn accumulates as free organic C in the sand-size fraction.