Bruun Sander, Harmer Sarah L, Bekiaris Georgios, Christel Wibke, Zuin Lucia, Hu Yongfeng, Jensen Lars Stoumann, Lombi Enzo
Department of Plant and Environmental Sciences, University of Copenhagen, Thorvaldsensvej 40, DK-1871, Frederiksberg C, Denmark.
School of Chemical and Physical Sciences, Flinders University, Bedford Park, SA, 5042, Australia.
Chemosphere. 2017 Feb;169:377-386. doi: 10.1016/j.chemosphere.2016.11.058. Epub 2016 Nov 22.
Biochar application to agricultural land has been proposed as a means for improving phosphorus (P) availability in soil. The purpose of the current study was to understand how pyrolysis temperature affects P speciation in biochar and how this affects availability of P in the amended soil. Biochar was produced at different temperatures from digestate solids. The primary species of P in digestate solids were simple calcium phosphates. However, a high co-occurrence of magnesium (Mg) and P, indicated that struvite or other magnesium phosphates may also be important species. At low temperatures, pyrolysis had little effect on P speciation; however, as the temperature increased above 600 °C, the P gradually became more thermodynamically stable in species such as apatite. At very high temperatures above 1000 °C, there were indications of reduced forms of P. Biochar production decreased the immediate availability of P in comparison with the original digestate solids. However, for biochar produced at low temperatures, availability quickly increased to the same levels as in the digestate solids. For biochar produced at higher temperatures, availability remained depressed for much longer. The low availability of P in the biochar produced at high temperatures can probably be explained by the formation of less soluble P species in the biochar. In contrast, the transient decrease of availability of the P in the biochar produced at low temperatures can be explained by mechanisms, such as sorption on biochar, which gradually decreases because of oxidation of the biochar surfaces or changes in pH around the biochar particles.
将生物炭施用于农田已被提议作为提高土壤中磷(P)有效性的一种方法。本研究的目的是了解热解温度如何影响生物炭中的磷形态,以及这如何影响改良土壤中磷的有效性。生物炭由消化固体在不同温度下制备而成。消化固体中磷的主要形态是简单的磷酸钙。然而,镁(Mg)和磷的高共现表明鸟粪石或其他磷酸镁也可能是重要形态。在低温下,热解对磷形态影响很小;然而,当温度升至600℃以上时,磷在磷灰石等形态中逐渐变得热力学上更稳定。在1000℃以上的非常高温度下,有迹象表明存在还原态的磷。与原始消化固体相比,生物炭的生产降低了磷的即时有效性。然而,对于低温制备的生物炭,有效性很快增加到与消化固体相同的水平。对于高温制备的生物炭,有效性在更长时间内仍处于较低水平。高温制备的生物炭中磷有效性低可能是由于生物炭中形成了溶解度较低的磷形态。相比之下,低温制备的生物炭中磷有效性的短暂下降可以通过诸如生物炭吸附等机制来解释,这种吸附会由于生物炭表面的氧化或生物炭颗粒周围pH值的变化而逐渐降低。