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施用聚磷酸铵的紫色土壤对磷的吸附-解吸特征

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[目的]探讨施用不同聚合度分布的聚磷酸铵(APP)土壤对磷的吸附-解吸特征及其与施用传统正磷酸盐磷酸一铵(MAP)和磷酸二铵(DAP)土壤的差异,为APP的高效利用提供理论依据.[方法]分别以3种APP(18-58-APP、16-60-APP和11-37-APP,N-P2O5-K2ø分别为18-58-0、16-60-0和11-37-0,聚合度分布分别为1-2、14和1-7)、MAP和DAP为供试肥料,在石灰性和酸性紫色土壤进行56 d培养,测定各处理土壤磷的吸附-解吸特征和土壤理化性质.[结果]Langmuir和Freundlich方程均能很好地拟合两种紫色土壤对磷的吸附特征(R2=0.825~0.997).在石灰性紫色土壤中,与施用MAP和DAP 土壤相比,施用APP 土壤对磷的吸附率降低15.1%~20.7%,解吸率提高4.5%~164.9%;施用APP 土壤的Langmuir KL值、吸附自由能(|ΔG|)和Fre-undlich KF值分别降低20.4%~54.0%、3.3%~10.6%和23.8%~43.8%,土壤对磷的吸附结合力减弱,其中施用11-37-APP 土壤相应值的变幅最大(KL、|ΔG|和KF值分别降低40.8%~54.0%、7.2%~10.6%和43.6%~43.8%).在酸性紫色土壤中,施用不同磷肥对土壤磷的吸附-解吸特征影响不显著,但施用APP 土壤较施用MAP和DAP 土壤表现出降低磷吸附和促进磷解吸的趋势.相关分析表明,土壤pH、铁铝氧化物和土壤有效磷(Olsen-P)含量与石灰性紫色土壤磷素吸附参数显著相关;土壤Olsen-P与酸性紫色土壤磷素吸附参数显著相关.施用APP石灰性紫色土壤中络合态铁铝氧化物降低,游离态铁铝氧化物增加,对磷的吸附降低且解吸增加.与石灰性土壤相比,酸性紫色土壤的有效磷含量更低,对磷的吸附能力更强,使得其吸附-解吸特征在短期内受不同磷肥影响差异不明显.[结论]施用APP紫色土壤磷的吸附-解吸特征受土壤性质和自身聚和度分布的影响,在石灰性紫色土壤中变化显著,且以聚合度分布更广泛的11-37-APP对土壤磷素吸附-解吸特征的影响更显著.
Adsorption-desorption characteristics of phosphorus in purple soils applied with ammonium polyphosphate
[Objective]The study aimed to investigate the adsorption-desorption characteristics of phosphorus(P)in soils applied with ammo-nium polyphosphates(APPs)of different polymerization distribution,and to compare these characteristics with those of soils applied with tra-ditional orthophosphates(Monoammonium phosphate,MAP;Diammonium phosphate,DAP).It can provide a theoretical basis for the efficient use of APP.[Method]Three kinds of APP(18-58-APP,16-60-APP and 11-37-APP,whose N-P2O5-K2O were 18-58-0,16-60-0 and 11-37-0,and the distribution of polymerization degree were 1-2,1-4 and 1-7,respectively),MAP and DAP were used as test fertilizers.The fertiliz-ers were applied to calcareous and acid purple soils and then were incubated for 56 days.The adsorption-desorption characteristics of P and the physicochemical properties of the soils were determined.[Result]Both Langmuir and Freundlich equations fit the adsorption characteris-tics of P in the two purple soils well(R2=0.825-0.997).In the calcareous purple soil,compared with MAP-and DAP-treated soils,the APP-treated soil showed a 15.1%-20.7%decrease in P adsorption rate and a 4.5%-164.9%increase in desorption rate.The Langmuir KL,adsorption free energy(|ΔG|),and Freundlich KF values of the APP-treated soil decreased by 20.4%-54.0%,3.3%-10.6%,and 23.8%-43.8%,respectively,indicating a reduction in the binding force of soil for P.The 11-37-APP treated soil showed the largest chan-ges in these values(KL,|ΔG|and KF values were reduced by 40.8%-54.0%,7.2%-10.6%and 43.6%-43.8%,respectively).In acid purple soil,the impact of different P fertilizers on the adsorption-desoprtion characteristics of P was not significant,but APP-treated soil tended to reduce P adsorption and promote P desorption.Correlation analysis showed that pH,iron and aluminum oxides,and Olsen-P were significantly correlated with P adsorption parameters in calcareous purple soil and soil Olsen-P was significantly correlated with P adsorption parameters in acid purple soil.APP application in calcareous purple soil decreased complexed iron and aluminum oxides while increased free iron and aluminum oxides,resulting in decreased P adsorption and increased desorption.Compared to calcareous soil,acid purple soil had a lower available P content and a stronger adsorption capacity,making the adsorption-desorption characteristics less susceptible to the influence of different P fertilizers in the short term.[Conclusion]The adsorption-desorption characteristics of P in APP-treated purple soils are influ-enced by the soil properties and the APP's polymerization distribution.The significant changes are observed in calcareous purple soil,espe-cially for 11-37-APP with a broader polymerization distribution.

Ammonium polyphosphatePurple soilsAdsorptionDesorption

黄明慧、李洋、许德华、严正娟、王辛龙

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四川大学化学工程学院,成都 610065

聚磷酸铵 紫色土壤 吸附 解吸

国家自然科学基金项目

32172677

2024

西南农业学报
四川,云南,贵州,广西,西藏及重庆省(区,市)农科院

西南农业学报

CSTPCD北大核心
影响因子:0.679
ISSN:1001-4829
年,卷(期):2024.37(8)