Results 261 to 270 of about 570,170 (331)

Magnesium-mediated stress adaptation in plants: from physio-biochemical insights to climate-resilient agriculture. [PDF]

open access: yesFront Plant Sci
Sarraf M   +8 more
europepmc   +1 more source

Global variation in vegetation carbon use efficiency inferred from eddy covariance observations. [PDF]

open access: yesNat Ecol Evol
Luo X   +11 more
europepmc   +1 more source

Carbon storage in mountain cloud forest communities, Jalpan de Serra, Querétaro, México. [PDF]

open access: yesCarbon Balance Manag
Elizabeth FR   +4 more
europepmc   +1 more source

Dataset of physicochemical, microbiological, and plant root parameters of 135 soils from various urban land uses Blois city, France. [PDF]

open access: yesData Brief
Norini MP   +26 more
europepmc   +1 more source

Is soil basal respiration a good indicator of soil pollution?

Geoderma, 2016
Abstract 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
openaire   +2 more sources

Bioremediation with Compost of a Diesel Contaminated Soil: Monitoring by Dehydrogenase Activity and Basal Respiration

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
openaire   +3 more sources

Temperature Sensitivity (Q10) of Soil Basal Respiration as a Function of Available Carbon Substrate, Temperature, and Moisture

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
openaire   +2 more sources

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