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Carolina Merino

Researcher at University of La Frontera

Publications -  19
Citations -  422

Carolina Merino is an academic researcher from University of La Frontera. The author has contributed to research in topics: Soil organic matter & Organic matter. The author has an hindex of 7, co-authored 15 publications receiving 201 citations.

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Meta-analysis of heavy metal effects on soil enzyme activities

TL;DR: A meta-analysis found the activities of seven enzymes to decrease in response to soil contamination with Pb, Zn, Cd, Cu and As, and the much stronger impact of HMs on living microorganisms and their endoenzymes than on extracellular enzymes stabilized on clay minerals and organic matter.
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Environmental drivers and stoichiometric constraints on enzyme activities in soils from rhizosphere to continental scale

TL;DR: In this paper, the authors determine environmental controls of extracellular enzyme production, and hence on potential enzyme activities (Vmax) and substrate affinities (Km), and conclude that substrate availability for microorganisms mainly determined enzyme activity patterns on the continental scale by the humidity gradient.
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Soil enzymes and biological activity at different levels of organic matter stability

TL;DR: A greater stabilization capacity of MF in allophanic soils than in kaolinitic soils due to the amorphous minerals clay materials was confirmed, and an inverse and significant relationship between Al pyrophosphate (Al bound to SOM) and the C-CO2 in volcanic soil, whereas the same correlation did not occur in kaalinitic soil.
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Soil carbon controlled by plant, microorganism and mineralogy interactions.

TL;DR: In this article, the authors focus on the competition for available carbon in soil, limiting their analyses to the interaction at rhizospheric space, where most processes between microorganisms and mineral phase occurs.
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Effects of drying/rewetting on soil aggregate dynamics and implications for organic matter turnover

TL;DR: In this paper, the effects of drying and rewetting (D/W) on soil organic matter turnover were evaluated at 5 and 25°C after a 27-day incubation of undisturbed soil cores from a temperate forest.