Department of Civil and Environmental Engineering, University of Delaware, Newark, DE 19716, United States.
Department of Agriculture and Natural Resources, Delaware State University, Dover, DE 19901, United States.
Sci Total Environ. 2015 Apr 15;512-513:454-463. doi: 10.1016/j.scitotenv.2015.01.093. Epub 2015 Jan 30.
Phosphorus (P) may be immobilized and consequently the runoff loss risks be reduced if poultry litter (PL) is converted into biochar prior to land application. Laboratory studies were conducted to examine the water extractability of P in PL biochar and its release kinetics in amended soils. Raw PL and its biochar produced through 400°C pyrolysis were extracted with deionized water under various programs and measured for water extractable P species and contents. The materials were further incubated with a sandy loam at 20 g kg(-1) soil and intermittently leached with water for 30 days. The P release kinetics were determined from the P recovery patterns in the water phase. Pyrolysis elevated the total P content from 13.7 g kg(-1) in raw PL to 27.1 g kg(-1) in PL biochar while reduced the water-soluble P level from 2.95 g kg(-1) in the former to 0.17 g kg(-1) in the latter. The thermal treatment transformed labile P in raw PL to putatively Mg/Ca phosphate minerals in biochar that were water-unextractable yet proton-releasable. Orthophosphate was the predominant form of water-soluble P in PL biochar, with condensed phosphate (e.g., pyrophosphate) as a minor form and organic phosphate in null. Release of P from PL biochar in both water and neutral soils was at a slower and steadier rate over a longer time period than from raw PL. Nevertheless, release of P from biochar was acid-driven and could be greatly promoted by the media acidity. Land application of PL biochar at soil pH-incorporated rates and frequency will potentially reduce P losses to runoffs and minimize the adverse impact of waste application on aquatic environments.
如果在将家禽粪便(PL)施用于土地之前将其转化为生物炭,则可以固定磷(P),从而降低径流损失的风险。进行了实验室研究,以检查 PL 生物炭中 P 的水可提取性及其在改良土壤中的释放动力学。用去离子水提取原始 PL 和通过 400°C 热解产生的生物炭,并根据各种方案进行测量,以测量水可提取的 P 形态和含量。进一步将材料与砂壤土以 20 g kg(-1) 的土壤混合,并在 30 天内间歇性地用水淋洗。通过水相中 P 的回收模式确定 P 的释放动力学。热解将原始 PL 中的总 P 含量从 13.7 g kg(-1)提高到 PL 生物炭中的 27.1 g kg(-1),同时将水溶性 P 水平从前者的 2.95 g kg(-1)降低到后者的 0.17 g kg(-1)。热处理将原始 PL 中的易变 P 转化为生物炭中假定的 Mg/Ca 磷酸盐矿物,这些矿物是水不可提取的,但可释放质子。正磷酸盐是 PL 生物炭中水溶性 P 的主要形式,缩合磷酸盐(例如焦磷酸盐)是次要形式,而有机磷酸盐则不存在。与原始 PL 相比,PL 生物炭在水和中性土壤中的 P 释放速度更慢,更稳定,持续时间更长。然而,生物炭中的 P 释放是由酸驱动的,并且可以大大促进媒体的酸度。以土壤 pH 结合的速率和频率将 PL 生物炭施用于土地将有可能减少径流中的 P 损失,并最大程度地减少废物施用于水生环境的不利影响。