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