2020
DOI: 10.1016/j.envres.2020.109962
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NH4+-N/NO3−-N ratio controlling nitrogen transformation accompanied with NO2−-N accumulation in the oxic-anoxic transition zone

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Cited by 40 publications
(7 citation statements)
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“…As for the HAV rhizosphere, it has unique classes of bacteria with varied special functions. Especially, it tended to recruit the nitrite reduction microorganisms for keeping the soil NH 4 + –N utilization and plant NH 4 + –N uptake . Furthermore, the higher levels of low-molecular-weight organic acids (mainly maleic acid) in the HAV rhizosphere could enhance CIP bioavailability, leading to adverse impact on the growth and colonization of NOB and less production and utilization of NO 3 – –N. , Overall, the variety-specific bacterial communities greatly affect the rhizosphere utilization of N forms.…”
Section: Discussionmentioning
confidence: 99%
“…As for the HAV rhizosphere, it has unique classes of bacteria with varied special functions. Especially, it tended to recruit the nitrite reduction microorganisms for keeping the soil NH 4 + –N utilization and plant NH 4 + –N uptake . Furthermore, the higher levels of low-molecular-weight organic acids (mainly maleic acid) in the HAV rhizosphere could enhance CIP bioavailability, leading to adverse impact on the growth and colonization of NOB and less production and utilization of NO 3 – –N. , Overall, the variety-specific bacterial communities greatly affect the rhizosphere utilization of N forms.…”
Section: Discussionmentioning
confidence: 99%
“…Due to the low level of oxygen or depletion in paddy soils, the rate of ammonification is slower compared with upland soils [ 108 ]. The depletion of O 2 in soils not only slows down the ammonification but also limits the process of ammonium oxidation (NH 4 + to NO 3 − ) and the immobilization of N (microbial assimilation of NH 4 + , i.e., the conversion of inorganic N to organic N), which leads to the accumulation of NH 4 + in soils [ 109 ].…”
Section: Hms and Soil N Transformationmentioning
confidence: 99%
“…The content of NH4 + -N in each treatment was analyzed by the phenol hypochlorite method. The content of NO 3− -N was analyzed using the UV spectroscopy method (Liu et al, 2020), and the sum of NH4 + -N and NO 3− -N content was taken as the content of available N. Ammonium acetate (1 mol L −1 NH 4 OAc pH 7.0) was used to extract available K, which was measured using a flame photometer (SherwoodM410). Available manganese (Mn), copper (Cu), and zinc (Zn) in the soil were determined by inductively coupled plasma-mass spectrometry.…”
Section: Data Collectionmentioning
confidence: 99%