Hao Zhuo, Dong Zhijie, Han Shuo, Zhang Aiping
Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing, China.
Front Plant Sci. 2022 Dec 14;13:1069627. doi: 10.3389/fpls.2022.1069627. eCollection 2022.
Promoting crop growth and regulating denitrification process are two main ways to reduce soil NO emissions in agricultural systems. However, how biochar and arbuscular mycorrhizal fungi (AMF) can regulate crop growth and denitrification in soils with different phosphorus (P) supplies to influence NO emission remains largely unknown.
Here, an eight-week greenhouse and one-year field experiments biochar and/or AMF (only in greenhouse experiment) additions under low and high P environments were conducted to characterize the effects on wheat (Triticum aestivum L.) growth and NO emission.
With low P supply, AMF addition decreased leaf Mn concentration (indicates carboxylate-releasing P-acquisition strategies), whereas biochar addition increased leaf Mn concentration, suggesting biochar and AMF addition regulated root morphological and physiological traits to capture P. Compared with low P supply, the high P significantly promoted wheat growth (by 16-34%), nutrient content (by 33-218%) and yield (by 33-41%), but suppressed soil NO emissions (by 32-95%). Biochar and/or AMF addition exhibited either no or negative effects on wheat biomass and nutrient content in greenhouse, and biochar addition promoted wheat yield only under high P environment in field. However, biochar and/or AMF addition decreased soil NO emissions by 24-93% and 32% in greenhouse and field experiments, respectively. This decrease was associated mainly with the diminished abundance of NO-producing denitrifiers (nirK and nirS types, by 17-59%, respectively) and the increased abundance of NO-consuming denitrifiers (nosZ type, by 35-65%), and also with the increased wheat nutrient content, yield and leaf Mn concentration.
These findings suggest that strengthening the plant-soil-microbe interactions can mitigate soil NO emissions via manipulating plant nutrient acquisition and soil denitrification.
促进作物生长和调节反硝化过程是农业系统中减少土壤一氧化氮(NO)排放的两种主要方式。然而,在不同磷(P)供应的土壤中,生物炭和丛枝菌根真菌(AMF)如何调节作物生长和反硝化作用以影响NO排放,目前仍知之甚少。
在此,进行了为期八周的温室试验和为期一年的田间试验,即在低磷和高磷环境下添加生物炭和/或AMF(仅在温室试验中),以表征其对小麦(Triticum aestivum L.)生长和NO排放的影响。
在低磷供应条件下,添加AMF降低了叶片锰浓度(表明释放羧酸盐的磷获取策略),而添加生物炭则提高了叶片锰浓度,这表明添加生物炭和AMF调节了根系形态和生理特征以获取磷。与低磷供应相比,高磷显著促进了小麦生长(提高16 - 34%)、养分含量(提高33 - 218%)和产量(提高33 - 41%),但抑制了土壤NO排放(降低32 - 95%)。在温室中,添加生物炭和/或AMF对小麦生物量和养分含量无影响或有负面影响,且在田间只有在高磷环境下添加生物炭才促进小麦产量。然而,在温室和田间试验中,添加生物炭和/或AMF分别使土壤NO排放降低了24 - 93%和32%。这种降低主要与产生NO的反硝化细菌(nirK和nirS类型,分别降低17 - 59%)丰度的减少以及消耗NO的反硝化细菌(nosZ类型,增加35 - 65%)丰度的增加有关,还与小麦养分含量、产量和叶片锰浓度的增加有关。
这些发现表明,通过操纵植物养分获取和土壤反硝化作用来加强植物 - 土壤 - 微生物相互作用可以减轻土壤NO排放。