农田耕作土壤CO2通量一直显著高于未耕作土壤(p<0.01)。农田土壤微生物量碳含量显著低于小叶章湿地(p<0.001)。在耕作后最初的1~3 d
湿地和农田土壤微生物量碳均没有显著的变化;之后
土壤微生物量碳迅速增加
显著高于未耕作土壤。观测时间内
耕作农田土壤微生物量碳含量始终显著高于未耕作土壤(p<0.01)。垦殖10年农田土壤耕作后
对土壤水溶性有机碳含量无显著影响。湿地耕作后
土壤水溶性有机碳迅速增加。在耕作后80 d内
土壤水溶性有机碳含量显著高于未耕作土壤(p<0.01)。之后
则低于未耕作土壤。
Abstract
Field experiment and laboratory simulated experiment were conducted to study the dynamic process of soil respiration flux
SMBC
basal respiration
metabolic quotient(qCO2) and DOC for Doyeuxia augustifolia wetland and cultivating-ten-year soil(agricultural soil) after tillage.The results showed that soil water content of Doyeuxia augustifolia wetland decreased significantly after soil tillage.Soil CO2 flux reached a peak in primary 1~2 days after tillage.CO2 flux of cultivated soil with tillage was higher all the time than that of soil without tillage(p<0.01).SMBC content of agricultural soil was higher significantly than that of Doyeuxia augustifolia wetland(p<0.001).SMBC content of wetland and agricultural soil had no significant difference in the primary 1~3 days after tillage.Since then SMBC content of soil with tillage increased rapidly and was higher than that of soil without tillage.For agricultural soil
SMBC content of soil with tillage was higher all through than that of soil without tillage. Soil tillage had no significant influence of DOC content on agricultural soil. However
DOC content of wetland increased rapidly after tillage.For wetland
DOC content of tillage was higher significantly than that of no tillage in primary 80 days(p<0.01)
while lower than that of no tillage after 80 days.