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Magnesium-mediated stress adaptation in plants: from physio-biochemical insights to climate-resilient agriculture. [PDF]
Sarraf M +8 more
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Global variation in vegetation carbon use efficiency inferred from eddy covariance observations. [PDF]
Luo X +11 more
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Carbon storage in mountain cloud forest communities, Jalpan de Serra, Querétaro, México. [PDF]
Elizabeth FR +4 more
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Artificial grassland establishment alters soil organic carbon fractions and <i>cbbL</i>-type carbon-sequestering microbial communities. [PDF]
Shan L +8 more
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Dataset of physicochemical, microbiological, and plant root parameters of 135 soils from various urban land uses Blois city, France. [PDF]
Norini MP +26 more
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Is soil basal respiration a good indicator of soil pollution?
Geoderma, 2016Abstract Metal(loid)s are common pollutants in soils, causing a significant toxicological risk to living organisms and to the ecosystems. Soil basal respiration (SBR) is broadly used as indicator of metal(loid) stress in polluted soils, although the correlation with toxicity gives in many cases contradictory results.
A. Romero-Freire +3 more
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Compost Science & Utilization, 2009
The effect of compost on hydrocarbon degradation was determined during a 120-d incubation period. An evaluation of soil basal respiration and dehydrogenase activity as a monitoring instrument for the bioremediation process of soil contaminated with commercial diesel-oil was carried out.
SAVIOZZI, ALESSANDRO +2 more
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The effect of compost on hydrocarbon degradation was determined during a 120-d incubation period. An evaluation of soil basal respiration and dehydrogenase activity as a monitoring instrument for the bioremediation process of soil contaminated with commercial diesel-oil was carried out.
SAVIOZZI, ALESSANDRO +2 more
openaire +3 more sources
Eurasian Soil Science, 2020
Basal respiration is one of the key indicators of soil C mineralization. Temperature sensitivity (Q10) of basal respiration is important for predicting changes in C mineralization due to warming. A modified methodology of Q10 determination is proposed. Soil samples were incubated at 25°C with periodic short-term (2 h) decline of temperature to 15°C and
M. S. Gromova +4 more
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Basal respiration is one of the key indicators of soil C mineralization. Temperature sensitivity (Q10) of basal respiration is important for predicting changes in C mineralization due to warming. A modified methodology of Q10 determination is proposed. Soil samples were incubated at 25°C with periodic short-term (2 h) decline of temperature to 15°C and
M. S. Gromova +4 more
openaire +2 more sources

