Soil carbon controlled by plant, microorganism and mineralogy interactions
Rhizosphere, a thin area of soil surrounding roots receiving carbon (C) exudation from plants, represents a site of intense competition for available C and nutrient between surface-reactive particles and soil microorganisms. This competition can reduce the amount of available C to a critical level,...
Guardado en:
Autores principales: | Merino,C, Nannipieri,P, Matus,F |
---|---|
Lenguaje: | English |
Publicado: |
Chilean Society of Soil Science / Sociedad Chilena de la Ciencia del Suelo
2015
|
Materias: | |
Acceso en línea: | http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-95162015000200004 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Enzymes of importance to rhizosphere processes
por: Gianfreda,L
Publicado: (2015) -
Availability of Mn, Zn and Fe in the rhizosphere
por: Rengel,Z
Publicado: (2015) -
Soil enzymes and biological activity at different levels of organic matter stability
por: Merino,C, et al.
Publicado: (2016) -
Rhizosphere-induced heavy metal(loid) transformation in relation to bioavailability and remediation
por: Seshadri,B, et al.
Publicado: (2015) -
Soil-Root-Microbe Interactions in the Rhizosphere: A Key to Understanding and Predicting Nutrient Bio availability to Plants
por: Hinsinger,P, et al.
Publicado: (2008)