Responses of soil microbial communities to manure and biochar in wheat cultivation of a rice-wheat rotation agroecosystem in East China

• Published in: Pedosphere 2023-12, Vol.33 (6), p.893-904
• Main Authors: MENG, Jun, LI, Wenjin, QIU, Yingbo, LI, Zhangtao, LI, Linze, LUO, Yu, GUO, Haipeng, YU, Yijun, SHAN, Shengdao, CHEN, Huaihai
• Format: Article
• Language: English
• ISSN: 1002-0160
• DOI: 10.1016/j.pedsph.2023.01.002

Soil contamination in agroecosystems remains a global environmental problem.Biochar has been suggested as an organic amendment to alleviate soil pollution,sequester carbon(C),and improve soil fertility.However,information on how bacterial and fungal communities in acidic bulk and rhizosphere soils respond to swine manure and its biochar is still lacking.In this study,biochar and swine manure were applied at two rates of 1.5 and 3 t ha-1 in a rice-wheat rotation field to assess how soil characteristics,especially pH and chemical element availability,correlate to compositional variations of bacteria and fungi in bulk and rhizosphere soils.Our results showed that high rates of biochar and manure promoted the bacterial richness in bulk and rhizosphere soils by increasing soil pH and reducing soil arsenic(As)and copper(Cu)availability.Compared with soil As and Cu availability,soil pH had opposite effects on beta diversity of both the bacterial and fungal communities.Specifically,biochar and swine manure applications stimulated the bacterial classes Gemmatimonadetes,Deltaproteobacteria,and Gammaproteobacteria by increasing soil pH and decreasing soil available chemical elements.Opposite trends were observed in fungal communities responding to biochar and manure.For example,biochar restrained the fungal class Eurotiomycetes by decreasing soil As and Cu availability,but manure inhibited Leotiomycetes mainly because of an increase in soil pH and a decrease in soil dissolved organic C.These suggest that both bacterial and fungal communities respond significantly to biochar and manure amendments in both bulk and rhizosphere soils,possibly because of their sensitive adaptation to variations in soil environmental factors,such as pH level and chemical element availability.