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Organic carbon additions: effects on soil bio‐physical and physico‐chemical properties
Author(s) -
Bhogal A.,
Nicholson F. A.,
Chambers B. J.
Publication year - 2009
Publication title -
european journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 1351-0754
DOI - 10.1111/j.1365-2389.2008.01105.x
Subject(s) - manure , total organic carbon , bulk density , topsoil , chemistry , soil carbon , crop residue , organic matter , nitrogen , soil organic matter , agronomy , zoology , environmental chemistry , environmental science , soil water , soil science , ecology , organic chemistry , biology , agriculture
Summary The effects of organic carbon (OC) additions from farm manures and crop residues on selected soil bio‐physical and physico‐chemical properties were measured at seven experimental sites, on contrasting soil types, with a history of repeated applications of farm manure or differential rates of inorganic fertilizer nitrogen (N). Repeated (> 7 years annual additions) and relatively large OC inputs (up to 65 t OC ha −1 ) were needed to produce measurable changes in soil properties, particularly physical properties. However, over all the study sites, there was a positive relationship between OC inputs and changes in total soil OC and ‘light’ fraction OC (LFOC), with LFOC providing a more sensitive indicator of changes in soil organic matter status. Total soil OC increased by an average of 3% for every 10 t ha −1 manure OC applied, whereas LFOC increased by c . 14%. The measured soil OC increases were equivalent to c . 23% of the manure OC applied (up to 65 t OC ha −1 applied over 9 years) and c . 22% of the crop residue OC applied (up to 32 t OC ha −1 over 23 years). The manure OC inputs (but not crop residue OC inputs) increased topsoil porosity and plant available water capacity, and decreased bulk density by 0.6%, 2.5% and 0.5% with every 10 t ha −1 manure OC applied, respectively. Both OC sources increased the size of the microbial biomass (11% increase in biomass C with 10 t OC ha −1 input), but only manure OC increased its activity (16% increase in the soil respiration rate with 10 t OC ha −1 input). Likewise, the potentially mineralizable N pool only increased with manure N inputs (14% increase with 1 t manure total N ha −1 ). However, these soil quality benefits need to be balanced with any potential environmental impacts, such as excessive nutrient accumulation, increased nitrate leaching and phosphorus losses and gaseous emissions to the atmosphere.