Soil organic matter evolution after the application of high doses of organic amendments in a Mediterranean calcareous soil

2012 ◽  
Vol 12 (8) ◽  
pp. 1257-1268 ◽  
Author(s):  
Sergio González-Ubierna ◽  
Ignacio Jorge-Mardomingo ◽  
Beatriz Carrero-González ◽  
María Teresa de la Cruz ◽  
Miguel Ángel Casermeiro
2017 ◽  
Vol 423 (1-2) ◽  
pp. 363-373 ◽  
Author(s):  
Emily E. Oldfield ◽  
Stephen A. Wood ◽  
Mark A. Bradford

2020 ◽  
Author(s):  
Beatrice Giannetta ◽  
Ramona Balint ◽  
Daniel Said-Pullicino ◽  
César Plaza ◽  
Maria Martin ◽  
...  

<p>Redox-driven changes in Fe crystallinity and speciation may affect soil organic matter (SOM) stabilization and carbon (C) turnover, with consequent influence on global terrestrial soil organic carbon (SOC) cycling.<span> </span>Under reducing conditions, increasing concentrations of Fe(II) released in solution from the reductive dissolution of Fe (hydr)oxides may accelerate ferrihydrite transformation, although our understanding of the influence of SOM on these transformations is still lacking.<span> </span></p><p>Here, we evaluated abiotic Fe(II)-catalyzed mineralogical changes in Fe (hydr)oxides in bulk soils and size-fractionated SOM pools (for comparison, fine silt plus clay, FSi+Cl, and fine sand, FSa) of an agricultural soil, unamended or amended with biochar, municipal solid waste compost, and a combination of both.<span> </span></p><p>FSa fractions showed the most significant Fe(II)-catalyzed ferrihydrite transformations with the consequent production of well-ordered Fe oxides irrespective of soil amendment, with the only exception being the compost-amended soils. In contrast, poorly crystalline ferrihydrite still constituted <em>ca. </em>45% of the FSi+Cl fractions of amended soils, confirming the that the higher SOM content in this fraction inhibits atom exchange between aqueous Fe(II) and the solid phase. Building on our knowledge of Fe(II)-catalyzed mineralogical changes in simple systems, our results evidenced that the mechanisms of abiotic Fe mineral transformations in bulk soils depend on Fe mineralogy, organic C content and quality, and organo-mineral associations that exist across particle-size SOM pools. Our results underline that in the fine fractions the increase in SOM due to organic amendments can contribute to limiting abiotic Fe(II)-catalyzed ferrihydrite transformation, while coarser particle-size fractions represent an understudied pool of SOM subjected to Fe mineral transformations.<span> </span></p>


2007 ◽  
Vol 170 (2) ◽  
pp. 234-243 ◽  
Author(s):  
Sheng-Mao Yang ◽  
Sukhdev S. Malhi ◽  
Feng-Min Li ◽  
Dong-Rang Suo ◽  
Ming-Gang Xu ◽  
...  

2013 ◽  
Vol 17 (24) ◽  
pp. 2998-3005 ◽  
Author(s):  
Riccardo Scotti ◽  
Pellegrino Conte ◽  
Anne Berns ◽  
Giuseppe Alonzo ◽  
Maria Rao

2016 ◽  
Vol 124 ◽  
pp. 139-148 ◽  
Author(s):  
Olsen Rainness Mouloubou ◽  
Pascale Prudent ◽  
Stéphane Mounier ◽  
Jean-Luc Boudenne ◽  
Madi Guirema Abaker ◽  
...  

Chemosphere ◽  
2007 ◽  
Vol 68 (7) ◽  
pp. 1245-1253 ◽  
Author(s):  
Julien Sebastia ◽  
Jérôme Labanowski ◽  
Isabelle Lamy

1969 ◽  
Vol 100 (2) ◽  
pp. 123-140
Author(s):  
Ian C. Pagán-Roig ◽  
Joaquín A. Chong ◽  
José A. Dumas ◽  
Consuelo Estévez de Jensen

The objective of this work was to measure the effects of repeated short-term organic amendments that we termed soil treatment management cycles (STMC) on physical and biological properties of a San Antón series soil. Each STMC lasted 60 days and consisted of incorporating 5% organic matter from coffee pulp compost; the planting, growth and incorporation of an intercrop of four green manure species; and the application of mycorrhizae and compost tea. The treatments were labeled: CL0, CL1, CL2 and CL3; where CL0 was the control, CL1 received one STMC, CL2 and CL3 received two and three STMC, respectively. The STMC intended to mimic the overall effect of a sustainable agricultural system, not to measure the individual effects of the practices. All treatments (CL1, CL2, CL3) showed an increase in soil organic matter (p≤0.05). When compared to the CL0 control, saturated hydraulic conductivity increased and bulk density decreased in all soils. Soil macroporosity was significantly increased by CL2 and CL3. Soil aggregate stability increased in CL1, CL2 and CL3 plots. Microbial biomass C increased in treatment CL3, and microbial biomass N increased in CL2 and CL3. The production of stable aggregates was correlated to humic acid content and positively influenced all other physical parameters assessed in this study. The STMC had a positive impact on soil properties by increasing the soil organic matter as well as the humic acid fraction. Soil macroporosity, defined as porosity with radius > 38 µm, was significantly increased by treatments CL2 and CL3. All of the organic matter fractions, including total organic matter, humic acid content, microbial biomass C and microbial biomass N were significantly increased by one or more STMC.


2020 ◽  
Vol 21 (1) ◽  
pp. 148-162
Author(s):  
Samar Fatima ◽  
Muhammad Riaz ◽  
Mohammad I. Al-Wabel ◽  
Muhammad Saleem Arif ◽  
Tahira Yasmeen ◽  
...  

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