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生物炭与磷施肥对盐碱性土壤中磷有效性和植物产量的负交互作用。

Negative interactive effects between biochar and phosphorus fertilization on phosphorus availability and plant yield in saline sodic soil.

机构信息

Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai 264003, China.

Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai 264003, China; University of Chinese Academy of Sciences, Beijing 100049, China.

出版信息

Sci Total Environ. 2016 Oct 15;568:910-915. doi: 10.1016/j.scitotenv.2016.06.079. Epub 2016 Jun 18.

Abstract

Little is known about the interactive effects between biochar application and phosphorus (P) fertilization on plant growth and P uptake. For this purpose, five wheat straw biochars (produced at 25°C, 300°C, 400°C, 500°C and 600°C for 4h) with equal P (36mgkg(-1)) amount, with and without additional P fertilization (100mgkg(-1)) were applied in a pot experiment to investigate the growth of Suaeda salsa and their uptake of P from biochar and P fertilization amended saline sodic soil. Soil P fractions, dry matter yield, and plant P concentrations were determined after harvesting 90days. Our results confirmed that relatively lower pyrolysis temperature (<400°C) biochar retained P availability and increased plant growth. The plant P concentration was significantly correlated with NaHCO3-Pi (P<0.05), and NaOH-Pi (P<0.1) during early incubation time (4days) for biochar amended soil. As revealed by statistical analysis, a significant (P<0.05) negative (antagonistic) interaction occurred between biochar and P fertilization on the biomass production and plant P concentration. For plant biomass, the effects size of biochar (B), P, and their interaction followed the order of B×P (0.819)>B (0.569)≈P (0.568) based on the partial Eta squared values whereas the order changed as P (0.782)>B (0.562)>B×P (0.515) for plant P concentration. When biochar and P fertilization applied together, phosphate precipitation/sorption reaction occurred in saline sodic soil which explained the decreased plant P availability and plant yield in saline sodic soil. The negative interaction effects between biochar and P fertilization indicated limited utility value of biochar application in saline sodic soil.

摘要

关于生物炭应用和磷(P)施肥对植物生长和 P 吸收的相互作用影响知之甚少。为此,在盆栽试验中,将 5 种小麦秸秆生物炭(在 25°C、300°C、400°C、500°C 和 600°C 下分别制备 4 小时)以相同的 P(36mgkg(-1))含量施加到添加和不添加额外 P 施肥(100mgkg(-1))的盐渍苏打土壤中,以研究盐生獐茅的生长及其对生物炭和 P 施肥添加的盐渍苏打土壤中 P 的吸收。收获 90 天后,测定土壤 P 形态、干物质产量和植物 P 浓度。我们的结果证实,相对较低的热解温度(<400°C)生物炭保留了 P 的有效性并增加了植物生长。在生物炭添加土壤的早期培养时间(4 天)内,植物 P 浓度与 NaHCO3-Pi(P<0.05)和 NaOH-Pi(P<0.1)显著相关。统计分析表明,生物炭和 P 施肥对生物量生产和植物 P 浓度的相互作用具有显著的(P<0.05)负(拮抗)相互作用。对于植物生物量,根据偏 Eta 平方值,生物炭(B)、P 和它们的相互作用的效应大小顺序为 B×P(0.819)>B(0.569)≈P(0.568),而对于植物 P 浓度,该顺序变为 P(0.782)>B(0.562)>B×P(0.515)。当生物炭和 P 施肥同时施加时,在盐渍苏打土壤中发生了磷酸盐沉淀/吸附反应,这解释了盐渍苏打土壤中植物 P 有效性和植物产量的降低。生物炭和 P 施肥之间的负相互作用表明,在盐渍苏打土壤中应用生物炭的有限实用价值。

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