State Key Laboratory of Subtropical Silviculture, Zhejiang A&F University, Lin'an 311300, Zhejiang, China; Zhejiang Provincial Collaborative Innovation Center for Bamboo Resources and High-efficiency Utilization, Zhejiang A&F University, Lin'an 311300, Zhejiang, China; School of Environmental and Resources Science, Zhejiang A&F University, Lin'an 311300, Zhejiang, China; 442 Earth Sciences Building, Department of Renewable Resources, University of Alberta, Edmonton T6G 2E3, Canada.
State Key Laboratory of Subtropical Silviculture, Zhejiang A&F University, Lin'an 311300, Zhejiang, China; Jiangsu Key Laboratory for Molecular and Medical Biotechnology, College of Life Sciences, Nanjing Normal University, Nanjing, China.
Sci Total Environ. 2020 May 1;715:136846. doi: 10.1016/j.scitotenv.2020.136846. Epub 2020 Jan 22.
The use of exogenous silicon (Si) amendments, such as Si fertilizers and biochar, can effectively increase crop Si uptake and the formation of phytoliths, which are siliceous substances that are abundant in numerous plant species. Phytolith-occluded carbon (C) (PhytOC) accumulation in soil plays an important role in long-term soil organic C (SOC) storage. Nevertheless, the effects of both Si fertilizer and biochar application on PhytOC sequestration in forest plant-soil systems have not been studied. We investigated the impact of Si fertilizer and biochar applications on 1) the PhytOC pool size, the solubility of plant and soil phytoliths, and soil PhytOC in soil physical fractions (light (LFOM) and heavy fractions of organic matter (HFOM)) in Moso bamboo (Phyllostachys pubescens) forests; and 2) the relationships among plant and soil PhytOC concentrations and soil properties. We used a factorial design with three Si fertilizer application rates: 0 (S0), 225 (S1) and 450 (S2) kg Si ha, and two biochar application rates: 0 (B0) and 10 (B1) t ha. The concentrations of PhytOC in the bamboo plants and topsoil (0-10 cm) increased with increasing Si fertilizer addition, regardless of biochar application. Biochar addition increased the soil PhytOC pool size, as well as the LFOM- and HFOM-PhytOC fractions, regardless of Si fertilizer application. The Si fertilizer application increased or had no effect on soil phytolith solubility with or without biochar application, respectively. Soil PhytOC was correlated with the concentration of soil organic nitrogen (R = 0.32), SOC (R = 0.51), pH (R = 0.28), and available Si (R = 0.23). Furthermore, Si fertilizer application increased plant and soil PhytOC by increasing soil available Si. Moreover, biochar application increased soil PhytOC concentration in LFOM-PhytOC and the unstable fraction of PhytOC. We conclude that Si fertilizer and biochar application promoted PhytOC sequestration in the plant-soil system and changed its distribution in physical fractions in the Moso bamboo plantation in subtropical China.
外源硅(Si)改良剂(如硅肥和生物炭)的使用可以有效地增加作物对硅的吸收和形成植硅体,植硅体是许多植物物种中丰富的硅质物质。土壤中植硅体结合碳(PhytOC)的积累在长期土壤有机碳(SOC)储存中起着重要作用。然而,硅肥和生物炭的应用对森林植物-土壤系统中 PhytOC 的固存影响尚未得到研究。我们研究了硅肥和生物炭的应用对 1)毛竹林(Phyllostachys pubescens)土壤中植硅体库大小、植物和土壤植硅体的溶解度以及土壤物理部分(LFOM 和 HFOM)中的土壤植硅体结合碳(PhytOC)和 2)植物和土壤植硅体浓度与土壤性质之间的关系的影响。我们采用了一个三因素设计,包括三个硅肥施用量:0(S0)、225(S1)和 450(S2)kg Si ha,以及两个生物炭施用量:0(B0)和 10(B1)t ha。无论生物炭的应用如何,随着硅肥施用量的增加,竹子植物和表土(0-10cm)中的 PhytOC 浓度均增加。生物炭的添加增加了土壤 PhytOC 库大小,以及 LFOM 和 HFOM-PhytOC 部分,无论是否施加硅肥。硅肥的施用分别增加或没有影响土壤植硅体的溶解度,而生物炭的施用则增加或没有影响土壤植硅体的溶解度。土壤 PhytOC 与土壤有机氮浓度(R=0.32)、SOC(R=0.51)、pH(R=0.28)和有效硅(R=0.23)呈正相关。此外,硅肥的施用通过增加土壤有效硅来增加植物和土壤 PhytOC。此外,生物炭的应用增加了 LFOM-PhytOC 和不稳定的植硅体结合碳。我们得出结论,硅肥和生物炭的施用促进了毛竹林植物-土壤系统中 PhytOC 的固存,并改变了其在物理部分的分布。