2007年6月至2009年10月,采用静态箱/气相色谱法测定了不同采伐干扰(皆伐后农作、皆伐后造林、50%强度采伐、25%强度采伐和对照)条件下,东北地区典型次生林的土壤CH。通量.结果表明:研究样地的土壤均为CH。的吸收汇.采伐干扰降低了土壤的CH。吸收能力,不同处理样地土壤的CH。吸收通量大小依次为:对照(一85.03μgCH。·m-2·h-1)〉50%强度采伐(-80.31μgCH4·m-2·h-1)〉25%强度采伐(-70.97μgCH4·m-2·h。)〉皆伐后农作(-65.57μgCH。·m-2·h-1)〉皆伐后造林(-62.02μgCH。·m-1 h。).各处理样地土壤CH。吸收通量的季节动态相似,均表现为生长季吸收值较高,冬季较低.采伐干扰后各处理的土壤温度、土壤湿度、土壤硝态氮和铵态氮含量均增加,而土壤CH。吸收通量与土壤温度呈显著二次相关,与土壤含水量呈线性负相关.次生林采伐后土壤含水量、土壤铵态氮和硝态氮含量的增加是土壤CH。吸收通量降低的重要控制因子.
From June, 2007 to October, 2009, a measurement with static chamber / gas chromato- graph techniques was conducted on the soil CH4 flux in a typical secondary hardwood forest in North- east China under the effects of different harvest disturbances, i. e. , uncut (control), clear cutting (including both farming and reforestation after clear cutting), 50% stand volume removed, and 25% stand volume removed. In all of the four treatments, the soil was the sink of atmospheric CH4, but cutting decreased the soil CH4 uptake flux, with the order of uncut ( -85.03 pLg CH4 ~ m-2 ~ h-1 ) 〉 50% stand volume removed (-80. 31 p,g CH4 ~ m-2 ~ h-1) 〉 25% stand volume removed ( -70.97 Ixg CH4 ~ m-2h-1 ) 〉 farming after clear cutting ( -65.57 pLg CH4 ~ m-2 ~ h-1 ) 〉 refores- tation after clear cutting ( -62.02 p.g CH4 ~ m-2 ~ h-1 ). During the study period, the seasonal pat- terns of the soil CH4 uptake flux in all treatments were similar, with a higher value in growth season and a lower one in winter. After the harvest disturbance, the soil temperature, humidity, and NO3--N, and NH4+-N contents were all increased, and the soil CH4 flux had a significant quadratic correlation with soil temperature, and a negative linear correlation with soil moisture content. It was suggested that the increase of the soil moisture, NO3--N, and NH4 ~-N contents after the forest har- vest was the main cause of the decrease of the soil CH4 uptake flux.