首页|长期施肥改变玉米大豆轮作/连作黑土农田酸化速率和酸中和容量

长期施肥改变玉米大豆轮作/连作黑土农田酸化速率和酸中和容量

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为探明不同种植制度和施肥措施对黑土酸化指标的影响及酸缓冲机制,依托东北旱田黑土肥力监测长期定位试验,研究了大豆连作(CS)、玉米连作(CC)以及玉米大豆轮作下玉米施化肥-大豆施化肥(CCF SCF)、玉米施化肥+秸秆还田-大豆不施化肥+秸秆还田(CCR SNOR)、玉米施化肥-大豆不施化肥(CCF SNOF)、玉米施化肥-大豆施1/2化肥(CCF S1/2CF)以及玉米施化肥-大豆施有机肥(CCF SDM)7个处理在第9年和第10年的土壤酸化速率(SAR)和酸中和容量(ANC)的变化,并利用二次多项式模型拟合酸滴定曲线,以pH 5。0和pH 4。5为参比计算了土壤ANC以及酸缓冲容量(ABC)。结果发现:相比于试验土壤本底值,试验第9年和第10年SAR变化幅度为-0。019~-0。097 ΔpH/a,其中CCF SDM处理的SAR在两年中变化最小(-0。021和-0。019 ΔpH/a);试验第9年CCF SCF、CCR SNOR、CCF SNOF、CCF S1/2CF和CCF SDM处理的土壤ANCpH5。0是试验第10年的1。11~1。77倍;土壤ANCpH4。5变化趋势与ANCpH5。0相一致。方差分解分析显示,土壤有机质和盐基离子总量是影响土壤ANC变化的主要因素,二者分别解释了试验处理第9年和第10年土壤ANC和ABC变化的63。44%和43。67%。综上可见,施化肥降低土壤酸中和容量,加速土壤酸化,而有机肥施用可通过提高土壤有机质和盐基离子总量提高黑土酸中和容量。
Long-term Fertilizer Application Alters Acidification Rate and Acid-Neutralizing Capacity in Corn and Soybean Rotational/Continuous Cropping Systems of Mollisol Field
In this study,to explore the effects of different cropping systems and fertilization practices on acidification indexes and acid buffering mechanisms in black soil,based on the Northeast Dryland Black Soil Fertility Monitoring Long-term Positioning Experiment Station,soil acidification rate(SAR)and soil acid-neutralizing capacity(ANC)under following seven treatments were investigated:continuous soybean with chemical fertilizer(CS),continuous corn with chemical fertilizer(CC),and corn-soybean rotation treatments including both corn and soybean with chemical fertilizer(CCF SCF),corn with chemical fertilizer plus straw return while soybean without chemical fertilizer but plus straw return(CCR SNOR),corn with chemical fertilizer while soybean without chemical fertilizer(CCF SNOF),corn with chemical fertilizer while soybean with 1/2 chemical fertilizer(CCF S1/2CF),corn with chemical fertilizer while soybean with dairy manure(CCF SDM).Soil ANC and acid-buffering capacity(ABC)at pH 5.0 and pH 4.5 were further calculated by using quadratic curve fitting model as references.The results showed that the change of SAR ranged from-0.019--0.097 ΔpH/a compared to the background pH after 9-and 10-year experimentation.Changes of SAR were lowest under CCF SDM in both two years(-0.021 and-0.019 ΔpH/a).Moreover,soil ANCpH5.0 in 9th year was 1.11-1.77 times compared with in 10th year under CCF SCF,CCR SNOR,CCF SNOF,CCF S1/2CF,and CCF SDM.The trends of ANCpH4.5 was consistent with ANCpH5.0.Variation partitioning analysis showed that soil organic matter(SOM)and the sum of exchangeable base(SEB)were the main factors affecting the changes in soil ANC,and both explained 63.44%and 43.67%of soil ANC and ABC variations after 9 and 10 years,respectively.In conclusion,chemical fertilizer application decreased soil ANC and accelerated soil acidification,while organic fertilizer application increased soil ANC by increasing SOM and SEB.

Black soilSoil acidification rate(SAR)Acid titration curveSoil acid-neutralizing capacity(ANC)

徐影、李彦生、刘晓冰、金剑、于镇华

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中国科学院东北地理与农业生态研究所黑土区农业生态重点实验室,哈尔滨 150081

中国科学院大学,北京 100049

黑土 土壤酸化速率 酸滴定曲线 土壤酸中和容量

国际大科学计划培育专项项目

131323KYSB20210004

2024

土壤
中国科学院南京土壤研究所

土壤

CSTPCD北大核心
影响因子:1.052
ISSN:0253-9829
年,卷(期):2024.56(4)