2016
DOI: 10.1007/s00374-016-1090-z
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How methane feedback response influence redox processes in a tropical vertisol

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Cited by 8 publications
(6 citation statements)
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“…In simulated experiments an increase in methane concentration in atmosphere resulted in a doubling of apparent CH 4 consumption rate (Mohanty et al, 2016). Methanotrophs and heterotrophs increased and there was increase in potential denitrification rate, potential iron and sulfate reduction rate.…”
Section: Microbiology Of Climate Changementioning
confidence: 95%
See 1 more Smart Citation
“…In simulated experiments an increase in methane concentration in atmosphere resulted in a doubling of apparent CH 4 consumption rate (Mohanty et al, 2016). Methanotrophs and heterotrophs increased and there was increase in potential denitrification rate, potential iron and sulfate reduction rate.…”
Section: Microbiology Of Climate Changementioning
confidence: 95%
“…Inoculation with high temperature and drought tolerant isolates significantly improved the yields of cluster bean, mungbean and pigeonpea under rain-fed conditions. Several Rhizobium isolates of pigeon pea, chickpea and soybean in acid soils analyzed by proteomic tools, which showed unique protein differences amongst acid-soil tolerant isolates (Dubey et al, 2016 ). Garg et al (2016) found seven biotypes of `berseem' rhizobia in Haryana soils of which two types were common in three districts showing some degree of endemism even in the high temperature arid soils.…”
Section: Rhizobial Diversitymentioning
confidence: 99%
“…For methanotrophs, the FM and FMR treatments resulted in higher abundances of pmoA genes than the other treatments (Figure 2a). Mohanty, Tiwari, Dubey, Ahirwar, and Kollah (2016) showed that methanotrophs are generally activated at high CH 4 concentrations. This was evidenced by the significantly positive relationship between the pmoA gene copy number and CH 4 emissions (Table S3 in Appendix S1).…”
Section: Effects Of Plant Residue Application On Methanogenic and Mmentioning
confidence: 99%
“…Based on the CH 4 changes (C-the final, and C 0 -the initial CH 4 concentration) during time (t), the average rates of CH 4 oxidation were calculated for all incubation periods using the following equation: CH 4 oxidation rate = (C-C 0 ) / t (Wnuk et al 2017). The equation C = C 0 e −kt , where k is the first-order kinetic constant (Mohanty et al 2016), was used for calculating the half-life value (t 1/2 ) expressed as days.…”
Section: Calculations and Statisticsmentioning
confidence: 99%
“…Arable soils are generally well aerated (Oenema 2001); therefore, they can be biological sinks for CH 4 . However, the methanotrophic activity of soils is controlled by a wide range of factors: CH 4 and O 2 as substrates (Bussmann et al 2006;Henckel et al 2000;Hernandez et al 2015;Li et al 2015;Mohanty et al 2016), soil properties and conditions such as organic C content and N availability and moisture, pH and temperature (Einola et al 2007;Huang et al 2016;Jäckel et al 2001;Kravchenko et al 2005), and human activities, such as grazing, deforestation, and fertilization (Bodelier 2011;Castillo et al 2017;Chen-rui et al 2003;Ho et al 2015;Köster et al 2017;Trimpler et al 2016).…”
Section: Introductionmentioning
confidence: 99%