Effect of N and P fertilization on the allocation and fixation of photosynthesized carbon in paddy soil

Potted rice seedlings independently treated with N, P, and NP were continuously13CO2 labeled to investigated the influence of N and P application on the contribution of photosynthesized C to the rhizosphere versus bulk soil and particulate organic matter (POM) versus mineral fraction (MIN). N and NP...

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Autores principales: Mostafa Zhran, Tida Ge, Yaoyao Tong, Zhenke Zhu, Yangwu Deng, Ahmed Fahmy, Ming Chen, Tin Mar Lynn, Jinshui Wu, Anna Gunina
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Publicado: Taylor & Francis Group 2021
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spelling oai:doaj.org-article:0a05d96b9bc54ceaa74d7ee0eb291f4a2021-12-02T17:23:22ZEffect of N and P fertilization on the allocation and fixation of photosynthesized carbon in paddy soil2332-887810.1080/20964129.2021.1941271https://doaj.org/article/0a05d96b9bc54ceaa74d7ee0eb291f4a2021-01-01T00:00:00Zhttp://dx.doi.org/10.1080/20964129.2021.1941271https://doaj.org/toc/2332-8878Potted rice seedlings independently treated with N, P, and NP were continuously13CO2 labeled to investigated the influence of N and P application on the contribution of photosynthesized C to the rhizosphere versus bulk soil and particulate organic matter (POM) versus mineral fraction (MIN). N and NP enhanced net assimilated 13C on day 14 (D14), with maximum C assimilation occurring on day 22 (D22) under NP. Aboveground biomass retained more 13C than belowground biomass for all treatments. 13C incorporation into the rhizosphere exceeded that in bulk soil, with the maximum (6–10%) found under N addition. Newly assimilated 13C incorporated into POM increased in the rhizosphere under N and NP conditions, whereas MIN remained largely unaffected. 13C-MBC proportion in the total microbial biomass C (MBC) pool revealed that N and NP stimulated microbial activity to a greater degree than P. The main portion of 13C in the rhizosphere and bulk soil was found in POM on D14, which decreased over time due to microbial utilization. Contrastingly, root-derived 13C in the MIN remained unchanged between sampling days, which indicates that the stabilization of rhizodeposits in this fraction might be the potential mechanism underlying SOM sequestration in paddy soils.Mostafa ZhranTida GeYaoyao TongZhenke ZhuYangwu DengAhmed FahmyMing ChenTin Mar LynnJinshui WuAnna GuninaTaylor & Francis Grouparticlepaddy soil13co2 continuous labelingfertilizationcarbon inputrhizospherebulk soilEcologyQH540-549.5ENEcosystem Health and Sustainability, Vol 7, Iss 1 (2021)
institution DOAJ
collection DOAJ
language EN
topic paddy soil
13co2 continuous labeling
fertilization
carbon input
rhizosphere
bulk soil
Ecology
QH540-549.5
spellingShingle paddy soil
13co2 continuous labeling
fertilization
carbon input
rhizosphere
bulk soil
Ecology
QH540-549.5
Mostafa Zhran
Tida Ge
Yaoyao Tong
Zhenke Zhu
Yangwu Deng
Ahmed Fahmy
Ming Chen
Tin Mar Lynn
Jinshui Wu
Anna Gunina
Effect of N and P fertilization on the allocation and fixation of photosynthesized carbon in paddy soil
description Potted rice seedlings independently treated with N, P, and NP were continuously13CO2 labeled to investigated the influence of N and P application on the contribution of photosynthesized C to the rhizosphere versus bulk soil and particulate organic matter (POM) versus mineral fraction (MIN). N and NP enhanced net assimilated 13C on day 14 (D14), with maximum C assimilation occurring on day 22 (D22) under NP. Aboveground biomass retained more 13C than belowground biomass for all treatments. 13C incorporation into the rhizosphere exceeded that in bulk soil, with the maximum (6–10%) found under N addition. Newly assimilated 13C incorporated into POM increased in the rhizosphere under N and NP conditions, whereas MIN remained largely unaffected. 13C-MBC proportion in the total microbial biomass C (MBC) pool revealed that N and NP stimulated microbial activity to a greater degree than P. The main portion of 13C in the rhizosphere and bulk soil was found in POM on D14, which decreased over time due to microbial utilization. Contrastingly, root-derived 13C in the MIN remained unchanged between sampling days, which indicates that the stabilization of rhizodeposits in this fraction might be the potential mechanism underlying SOM sequestration in paddy soils.
format article
author Mostafa Zhran
Tida Ge
Yaoyao Tong
Zhenke Zhu
Yangwu Deng
Ahmed Fahmy
Ming Chen
Tin Mar Lynn
Jinshui Wu
Anna Gunina
author_facet Mostafa Zhran
Tida Ge
Yaoyao Tong
Zhenke Zhu
Yangwu Deng
Ahmed Fahmy
Ming Chen
Tin Mar Lynn
Jinshui Wu
Anna Gunina
author_sort Mostafa Zhran
title Effect of N and P fertilization on the allocation and fixation of photosynthesized carbon in paddy soil
title_short Effect of N and P fertilization on the allocation and fixation of photosynthesized carbon in paddy soil
title_full Effect of N and P fertilization on the allocation and fixation of photosynthesized carbon in paddy soil
title_fullStr Effect of N and P fertilization on the allocation and fixation of photosynthesized carbon in paddy soil
title_full_unstemmed Effect of N and P fertilization on the allocation and fixation of photosynthesized carbon in paddy soil
title_sort effect of n and p fertilization on the allocation and fixation of photosynthesized carbon in paddy soil
publisher Taylor & Francis Group
publishDate 2021
url https://doaj.org/article/0a05d96b9bc54ceaa74d7ee0eb291f4a
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