Li Zimin, Guo Fengshan, Cornelis Jean-Thomas, Song Zhaoliang, Wang Xudong, Delvaux Bruno
Soil Science, Earth and Life Institute, Université catholique de Louvain (UCLouvain), Louvain-la-Neuve, Belgium.
School of Environment and Resources, Zhejiang Agricultural and Forestry University, Lin'an, China.
Front Plant Sci. 2020 Feb 18;11:67. doi: 10.3389/fpls.2020.00067. eCollection 2020.
Phytoliths are silica bodies formed in living plant tissues. Once deposited in soils through plant debris, they can readily dissolve and then increase the fluxes of silicon (Si) toward plants and/or watersheds. These fluxes enhance Si ecological services in agricultural and marine ecosystems through their impact on plant health and carbon fixation by diatoms, respectively. Fertilization increases crop biomass through the supply of plant nutrients, and thus may enhance Si accumulation in plant biomass. Si and phosphorus (P) fertilization enhance rice crop biomass, but their combined impact on Si accumulation in plants is poorly known. Here, we study the impact of combined Si-P fertilization on the production of phytoliths in rice plants. The combination of the respective supplies of 0.52 g Si kg and 0.20 g P kg generated the largest increase in plant shoot biomass (leaf, flag leaf, stem, and sheath), resulting in a 1.3-fold increase compared the control group. Applying combined Si-P fertilizer did not affect the content of organic carbon (OC) in phytoliths. However, it increased plant available Si in soil, plant phytolith content and its total stock (mg phytolith pot) in dry plant matter, leading to the increase of the total amount of OC within plants. In addition, P supply increased rice biomass and grain yield. Through these positive effects, combined Si-P fertilization may thus address agronomic (e.g., sustainable ecosystem development) and environmental (e.g., climate change) issues through the increase in crop yield and phytolith production as well as the promotion of Si ecological services and OC accumulation within phytoliths.
植硅体是在活植物组织中形成的硅质体。一旦通过植物残体沉积在土壤中,它们很容易溶解,然后增加硅(Si)向植物和/或流域的通量。这些通量分别通过对植物健康的影响和硅藻的固碳作用,增强了农业和海洋生态系统中的硅生态服务。施肥通过提供植物养分增加作物生物量,因此可能会增强植物生物量中硅的积累。硅和磷(P)施肥可提高水稻作物生物量,但它们对植物中硅积累的综合影响尚不清楚。在这里,我们研究了硅磷联合施肥对水稻植株中植硅体产生的影响。分别供应0.52 g Si/kg和0.20 g P/kg产生了最大的植株地上部生物量(叶、旗叶、茎和鞘)增加,与对照组相比增加了1.3倍。施用硅磷复合肥不影响植硅体中有机碳(OC)的含量。然而,它增加了土壤中植物有效硅、植物植硅体含量及其在干植物物质中的总存量(mg植硅体/盆),导致植物体内OC总量增加。此外,磷的供应增加了水稻生物量和籽粒产量。通过这些积极作用,硅磷联合施肥可能通过提高作物产量和植硅体产量,以及促进硅生态服务和植硅体内OC积累,解决农艺(如可持续生态系统发展)和环境(如气候变化)问题。