吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (4): 1204-1216.doi: 10.13278/j.cnki.jjuese.20200022
汤洁, 陈静书, 李昭阳, 王静静, 吕航
Tang Jie, Chen Jingshu, Li Zhaoyang, Wang Jingjing, Lü Hang
摘要: 为了研究不同盐碱程度旱田和水田土壤有机碳(SOC)矿化对氮、磷添加的响应,定量化其激发效应的大小和方向,选择了吉林西部3块盐碱旱田样地(H1,H2,H3)和3块盐碱水田样地(S1,S2,S3),采用实验室模拟培养,将无机营养素((NH4)2SO4、KNO3和KH2PO4)以7种形式添加到0~15 cm表层土壤样本中,在25 ℃恒温箱内连续监测32 d的CO2释放量,分析7种氮、磷添加处理对SOC矿化和激发效应的影响。结果表明:1)按7种处理形式分别添加200 mg/kg和1 000 mg/kg氮或磷,SOC矿化量和矿化速率均增加了158.5%~876.5%;同一添加物的质量分数越高,SOC矿化量越大,且随着培养时间延长,SOC矿化速率呈逐渐降低的趋势。2)在培养期间,各添加组均产生了正激发效应。3)在培养期间,部分处理组的SOC矿化、激发效应和碱化度表现出显著负相关性(显著性水平p<0.05)。碱化度越大,SOC矿化作用和激发效应越弱;矿化作用越大,正激发效应越低。4)与水田土壤相比,旱田SOC矿化和激发效应对添加氮、磷的响应更大。
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