Study of C, N, P and K Release from Residues of Newly Proposed Cover Crops in a Spanish Olive Grove

Cover crops (CC)s are increasingly employed by farmers in olive groves. Spontaneous soil cover is the most commonly used CC. Its continuous utilization changes ruderal flora. It is necessary to study new CCs. Living CCs provide C and nutrients to soil during decomposition. Information on this issue...

ver descrição completa

Detalhes bibliográficos
Autores: Rodríguez Lizana, Antonio, Repullo Ruibérriz De Torres, Miguel Ángel, Carbonell Bojollo, Rosa M., Moreno García, Manuel, Ordoñez Fernández, Rafaela
Formato: artículo
Estado:Versión publicada
Fecha de publicación:2020
País:España
Recursos:Universidad de Sevilla (US)
Repositorio:idUS. Depósito de Investigación de la Universidad de Sevilla
OAI Identifier:oai:idus.us.es:11441/100922
Acesso em linha:https://hdl.handle.net/11441/100922
https://doi.org/10.3390/agronomy10071041
Access Level:acceso abierto
Palavra-chave:Cover crops
Olive grove
Decomposition model
Nutrient release
Nitrogen
Carbon
Phosphorus
Potassium
Sinapis alba
Brachypodium distachyon
Descrição
Resumo:Cover crops (CC)s are increasingly employed by farmers in olive groves. Spontaneous soil cover is the most commonly used CC. Its continuous utilization changes ruderal flora. It is necessary to study new CCs. Living CCs provide C and nutrients to soil during decomposition. Information on this issue in olive groves is scarce. A 4-year field study involving grab sampling of Brachypodium distachyon, Sinapis alba and spontaneous CC residues was conducted to study C and nutrient release from cover crop residues. Throughout the decomposition cycles, C, N and P release accounted for 40 to 58% of the C, N and P amounts in the residues after mowing. Most K was released (80–90%). Expressed in kg per hectare, the release of C and N in Brachypodium (C: 4602, N: 181, P: 29, K: 231) and Sinapis (C: 4806, N: 152, P: 18, K: 195) was greater than that in spontaneous CC (C: 3115, N: 138, P: 21, K: 256). The opposite results were observed for K. The Rickman model, employed to estimate the amount of C, N and P in residues, yielded a good match between the simulated and measured values. In comparison to spontaneous CC, the newly proposed CCs have a higher potential to provide soil with C and N.