Humic substances and its distribution in coffee crop under cover crops and weed control methods

Abstract

Humic substances (HS) comprise the passive element in soil organic matter (SOM), and represent one of the soil carbon pools which may be altered by different cover crops and weed control methods. This study aimed to assess HS distribution and characteristics in an experimental coffee crop area subjected to cover crops and cultural, mechanical, and chemical weed control. The study was carried out at Londrina, in the state of Paraná, southern Brazil (23°21'30" S; 51°10'17" W). In 2008, seven weed control/cover crops were established in a randomized block design between two coffee rows as the main-plot factor per plot and soil sampling depths (0-10 cm, 10-20 cm, 20-30 cm and 30-40 cm) as a split-plot. HS were extracted through alkaline and acid solutions and analyzed by chromic acid wet oxidation and UV-Vis spectroscopy. Chemical attributes presented variations in the topsoil between the field conditions analyzed. Cover crop cutting and coffee tree pruning residues left on the soil surface may have interfered in nutrient cycling and the humification process. Data showed that humic substances comprised about 50 % of SOM. Although different cover crops and weed control methods did not alter humic and fulvic acid carbon content, a possible incidence of condensed aromatic structures at depth increments in fulvic acids was observed, leading to an average decrease of 53 % in the E 4 /E 6 ratio. Humin carbon content increased 25 % in the topsoil, particularly under crop weed-control methods, probably due to high incorporation of recalcitrant structures from coffee tree pruning residues and cover crops.

Solubilidade dos macronutrientes primários: nitrogênio, fósforo e potássio a partir dos resíduos vegetais

“…porte alto e arquitetura da planta cilíndrica (Matiello et al, 2005) que exigem espaçamento mais largos entre as linhas de plantio ou podas mais frequentes para não dificultar a circulação de máquinas (Carvalho et al, 2022). O aporte dos resíduos dos cafeeiros sobre o solo auxilia na qualidade da matéria orgânica do solo e na dinâmica das substâncias húmicas em um LATOSSOLO VERMELHO Distroférrico típico, textura muito argilosa do norte do estado do Paraná (Martins et al, 2016a, b).…”