Showing posts with label Humification; Young soil organic matter; Soil organic matter; Crop residue decomposition; Model. Show all posts
Showing posts with label Humification; Young soil organic matter; Soil organic matter; Crop residue decomposition; Model. Show all posts

Thursday, July 5, 2018

Cover Crops in the Production System


Cover crops in the Southeastern region of Buenos Aires, Argentina: effects on organic matter physical fractions and nutrient availability
In the Southeastern region of Buenos Aires province, soybean monoculture has led to a decline in soil organic matter (SOM) levels in soil, mostly the labile fractions. The reduction of SOM has a negative impact on the soil environment. Cover crops (CC) constitute an alternative to maintain or improve SOM levels. The aim of this study was to determine the effect of oat as CC on (a) the SOM dynamics and (b) the availability of macro- and micronutrients in a representative soil of the Southeastern region of Buenos Aires province. Total organic carbon (TOC) and nitrogen (TON), as well as their labile and mineral-associated fractions, and macro- and micronutrient availability were determined. The treatments were soybean monoculture with and without oat as cover crop. The increases in SOC and TON were 22.7% and 11%, respectively, when CC was included to the soybean monoculture. These increases were observed mostly in the labile fractions, with increases of 61.3 and 38.7% for the particulate coarse organic carbon (PCOf) and particulate fine organic carbon (PCOf), respectively, and 79.2% for the particulate coarse organic nitrogen (NOPg). Regarding the nutrients, an increase of 47.6% was observed in manganese (Mn) in the first 5 cm of soil depth, and a decrease in phosphorous (P) availability in the same soil layer due to its consumption and retention by CC. It can be conclude that CC presented a surface soil effect on the dynamic of SOM, increasing C, N, and available Mn contents, but decreasing soil P availability
Oat, Soybean monoculture, Particulate organic carbon and nitrogen

Beltrán M.J., H. Sainz Rozas, J.A. Galantini, R.I. Romaniuk, P. Barbieri. 2018. Cover crops in the Southeastern region of Buenos Aires, Argentina: effects on organic matter physical fractions and nutrient availability. Environmental Earth Sciences 77:428. DOI: 10.1007/s12665-018-7606-0.
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Tuesday, December 16, 2014

Humification and N mineralization of crop residues in semi-arid Argentina

Crop residues in the soil play a fundamental role in organic matter dynamics and have effects on numerous beneficial soil properties. The humification of residues depends on soil nutrient status and physical and meteorological conditions. The prediction of the humification rate and of the size and decomposition of fresh and humified soil organic matter has been attempted with equations and models which require several constants. To simplify the procedure, Janssen developed an equation which utilizes only one constant, allows to calculate the young (fresh) and old (humified) soil organic matter pools and predicts the production of available or mineralized nitrogen. The validity of Janssen's equation was tested in three production systems (a crop rotation and two tillage procedures) in a sandy-loam textured, thermic, entic Haplustoll soil in the pampean semi-arid region of Argentina. The model produced results compatible with actual field data, but information on soil available water was essential for fitting and interpreting the organic matter dynamics.

Galantini J.A., Rosell R.A., Andriulo A.E., Miglierina A.M., Iglesias J.O. 1992. Humification and N mineralization of crop residues in semi-arid Argentina. The Science of the Total Environment (Netherlands), 117/118: 263-270.
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