不同pH值生物质灰分K~+释放动力学分析

Q3 Agricultural and Biological Sciences
Wang Ka
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引用次数: 0

摘要

生物质灰是秸秆在800℃下燃烧产生的一种植物秸秆残渣。生物质灰含有大量的营养物质,包括磷(P)、钙(Ca)、镁(Mg),尤其是钾(K)。在生物质灰中,K主要以K2 SO4、KCl和K2 CO3的形式存在。近年来,生物质灰已被用于生产钾基肥料。然而,对生物质灰分K+释放的原理和机制研究较少。在利用生物质灰生产钾肥的新生产系统和方法中,pH值对K+的释放至关重要。以四种生物质灰(玉米秸秆、稻草、锯材和谷壳)为研究对象,通过乙酸铵(NH4 Ac)调节pH值为4、7和9,采用渗透交换法提取有效钾。本研究探讨了K+的累积释放量和释放速率,并利用3种动力学模型分析了4种生物质灰的K+释放动态。结果表明,在20 ~ 80 min内钾离子释放达到平衡,不同pH下钾离子释放总量差异显著,pH = 4时,总释放量为14.77 ~ 255.17 cmol·kg-1, pH = 7时为4.83 ~ 106.71 cmol·kg-1, pH = 9时为12.11 ~ 224.33 cmol·kg-1。各pH条件下总K+释放量显示,水稻秸秆释放K+最多,玉米秸秆和锯材次之,谷壳释放K+最少。相关性分析表明,总钾含量对K+释放时间和总释放量具有重要影响。释钾量与全钾含量的相关系数为0.991 ~ 0.997。不同类型生物量灰分的K+释放速率存在显著差异。这表明含钾量越大,K+释放量越大。这表明,交换液的pH和总钾含量不同,K+的平衡时间和释放量也不同。3种pH条件下,水稻秸秆和玉米秸秆的K+释放量依次为Q4、Q9、Q7,锯材和谷壳的K+释放量依次为Q9、Q4、Q7。3种pH条件下,生物质灰分总K+释放量的大小顺序为:水稻秸秆、锯材、谷壳、玉米秸秆。在平衡时间之前,各反应阶段的K+释放速度(v)与时间(lnt)呈对数相关。对于相同的生物质灰分,K+释放的最佳动力学模式随pH条件的变化而变化。pH = 4、7和9时,最佳模型分别为Elovich方程(EE)、Dual Constant Equation(DCE)和EE。在相同的pH条件下,EE和DCE是最能描述K+释放过程的模型,而抛物扩散(抛物扩散)是最不合适的模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of K~+ release kinetics of biomass ash with different pH
Biomass ash is a kind of plant straw residuum produced by combustion of straw at 800 ℃. Biomass ash contains lots of nutrients, including phosphorus(P), calcium(Ca), magnesium(Mg) and especially potassium(K). In biomass ash, K mainly occurs as K2 SO4, KCl and K2 CO3. In recent years, biomass ash has been used to produce potassium-based fertilizers. However, less work has been done on the principles and mechanisms of biomass ash K+ release. In the new production system and method proposed to produce potassium fertilizers from biomass ash, pH is critical for K+ release. This paper used four types of biomass ash(cornstalk, rice straw, sawn wood and chaff) with different pH of 4, 7 and 9 adjusted by ammonium acetate(NH4 Ac) to extract available K by the method of penetration exchange. This study discussed the cumulative quantity and rate of release of K+, and analyzed K+ release dynamics of four types of biomass ash using three kinetic models. The results indicated that K+ release attained equilibrium in 20-80 min with a total capacity of K+ release significantly different for different pH. Total K+ release capacity was 14.77-255.17 cmol·kg-1at pH of 4, 4.83-106.71 cmol·kg-1 at pH of 7 and 12.11-224.33 cmol·kg-1 at pH of 9. Total K+ release capacity under each pH condition showed that rice straw released the most K+, followed by cornstalk and sawn wood, while chaff released the least K+. Correlation analysis suggested that total K content of biomass ash was critical for the time and total capacity of K+ release. The correlation coefficient of released K+ amount and total K content was 0.991-0.997. A significant difference was noted in K+ release rate among biomass ash types. These implied that the greater content of K contain the more amount of K+ release. This indicated that equilibrium time and quantity of released K+ varied with pH and total K content of exchange solution. Under the three pH conditions, released K+ amounts(Q) of rice straw and cornstalk were in the order of Q4 Q9 Q7, while those of sawn wood and chaff were Q9 Q4 Q7. The order of total K+ release capacity of biomass ash was Q Rice straw QSawn wood QChaff QCornstalks under the three pH conditions. Before equilibrium time, K+ release velocity(v) was logarithmically related with time(lnt) during each reaction stage. For the same biomass ash, the optimal kinetic mode of K+ release changed with pH condition. The best models at pH of 4, 7 and 9 were Elovich Equation(EE), Dual Constant Equation(DCE) and EE, respectively. Under the same pH condition, the model that best described K+ release process was the EE and DCE, while the Parabolic Diffusion(PD) was the most inappropriate model.
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来源期刊
Chinese Journal of Eco-agriculture
Chinese Journal of Eco-agriculture Environmental Science-Ecology
CiteScore
2.70
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