ABSTRACT
Effect of Compost Application on Some Properties of a Volcanic Soil from Central South Chile

Pedro José Valarini1, Gustavo Curaqueo2, Alex Seguel2, Karina Manzano2, Rosa Rubio2, Pablo Cornejo2, and Fernando Borie2*
 

Soil compost application is a common soil management practice used by small farmers of Central-South Chile that produces positive effects on soil properties and also promotes presence and activity of arbuscular mycorrhizal fungi (AMF). This fungi form symbiosis with plant roots improving plant nutrition, as well as producing glomalin, a glycoprotein that has been associated with soil aggregation stability. Therefore, the aim of this study was to evaluate, in an Ultisol from Central-South Chile, the effect of different doses of compost on some soil characteristics at the end of the third year of a crop sequence including wheat (Triticum aestivum L.), bean (Phaseolus vulgaris L.), and grassland (Lolium multiflorum Lam. associated with Trifolium repens L.). Studied soil characteristics included chemical (pH, available-P, organic C), biological (C and N biomass, AMF spore number, root colonization percentage, mycelium length, and glomalin content), as well as physical parameters (water holding capacity [WHC], and water stable aggregates [WSA]). Results showed that, in general, compost application increased soil pH, mycorrizal roots, mycelium length, glomalin levels, and WSA. Significant relationships were found between C and N biomass, C biomass and WSA, C biomass and glomalin, WSA and WHC, among others. Results suggest that compost application to this type of soil is a feasible option as a fertilizer substitute, and a way to avoid soil erosion by small local farmers involved in organic agriculture.

Keywords: compost, glomalin, soil aggregation, Ultisol
1 EMBRAPA Meio Ambiente, Rodovia SP 340, km 127.5, Caixa Postal 69, Jaguariúna, São Paulo, Brasil.
2 Universidad de La Frontera, Facultad de Ingeniería, Ciencias y Administración, Casilla 54-D, Temuco, Chile.*Corresponding author (fborie@ufro.cl).