TY - JOUR
T1 - Interactions between periphytic biofilms and dissolved organic matter at soil-water interface and the consequent effects on soil phosphorus fraction changes
AU - Liu, Junzhuo
AU - Lu, Haiying
AU - Wu, Lirong
AU - Kerr, Philip G.
AU - Wu, Yonghong
N1 - Funding Information:
This work was supported by the National Natural Science Foundation of China ( 41977101 , 41825021 ), the Natural Science Foundation of Jiangsu Province , China ( BK20181511 , BE2020731 , BK20200057 ), and Chinese Academy of Sciences .
Publisher Copyright:
© 2021 Elsevier B.V.
PY - 2021/12/20
Y1 - 2021/12/20
N2 - Dissolved organic matter (DOM) plays vital roles in carbon and other nutrient transformation at soil-water interfaces (SWI) in paddy fields. It is associated with the growth and withering of periphytic biofilms. However, the interactions between DOM and periphytic biofilms remain largely unknown. In this study, a microcosm experiment with different initial DOM contents elucidated that the biomass, and biomass nitrogen and phosphorus contents were greatly influenced by humic-like substances (C2 and C3), while the growth of periphytic biofilms increased the contents of humic-like (C1 and C2) and tryptophan-like substances (C5) in soil. Moreover, the decomposition of periphytic biofilms significantly increased soil pH, DOM, C2, C3 and C5 contents, but caused decrease in Eh, with consequent reduce in water soluble phosphorus (WSP) and release of algal available phosphorus (AAP). Results from this study revealed how DOM interacts with periphytic biofilms and the consequent effects on changes of bioactive phosphorus fractions, and provide practical information for designing periphytic biofilm based biofertilizer from the perspective of soil DOM.
AB - Dissolved organic matter (DOM) plays vital roles in carbon and other nutrient transformation at soil-water interfaces (SWI) in paddy fields. It is associated with the growth and withering of periphytic biofilms. However, the interactions between DOM and periphytic biofilms remain largely unknown. In this study, a microcosm experiment with different initial DOM contents elucidated that the biomass, and biomass nitrogen and phosphorus contents were greatly influenced by humic-like substances (C2 and C3), while the growth of periphytic biofilms increased the contents of humic-like (C1 and C2) and tryptophan-like substances (C5) in soil. Moreover, the decomposition of periphytic biofilms significantly increased soil pH, DOM, C2, C3 and C5 contents, but caused decrease in Eh, with consequent reduce in water soluble phosphorus (WSP) and release of algal available phosphorus (AAP). Results from this study revealed how DOM interacts with periphytic biofilms and the consequent effects on changes of bioactive phosphorus fractions, and provide practical information for designing periphytic biofilm based biofertilizer from the perspective of soil DOM.
KW - 3D EEM
KW - Biomass decomposition
KW - Paddy soil
KW - PARAFAC
UR - http://www.scopus.com/inward/record.url?scp=85113341035&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85113341035&partnerID=8YFLogxK
U2 - 10.1016/j.scitotenv.2021.149708
DO - 10.1016/j.scitotenv.2021.149708
M3 - Article
C2 - 34438149
AN - SCOPUS:85113341035
SN - 0048-9697
VL - 801
SP - 1
EP - 9
JO - Science of the Total Environment
JF - Science of the Total Environment
M1 - 149708
ER -