Wang Ning, Wang Mei-ju, Li Shi-lan, Wang Nan-nan, Feng Fu-juan, Han Shi-jie
Ying Yong Sheng Tai Xue Bao. 2015 May;26(5):1297-305.
Broadleaved Korean pine mixed forest is the zonal climax vegetation in Northeast China and it plays a significant role in maintaining the ecological security. Changbai Mountains is a suitable region to study the positive and negative feedback mechanisms of temperate forest for precipitation variation. This study analyzed responses of soil microbial biomass carbon (SMBC) and microbial biomass nitrogen (SMBN) to precipitation variation (± 30%) in original broadleaved Korean pine mixed forest of Changbai Mountains. The results showed that, during the growing seasons (from May to September), the averages of SMBC and SMBN were 879.09 and 100.03 mg · kg(-1), respectively. Moreover, both of these two parameters gradually decreased with the soil depth. The contents of SMBC and SMBN all increased with the increasing precipitation, and the changes of SMBC and SMBN in the 0-5 cm soil layer were stronger than in the 5-10 cm soil layer. The value of SMBC/SMBN declined with the increase of precipitation. The precipitation variation significantly influenced the means of SMBC and SMBN. Compared with precipitation reduction, precipitation enhancement affected the indices much significantly. Both SMBC and SMBN showed similar seasonal patterns, which were the lowest in May, and after that, they increased and then decreased and increased again, showing 1-2 peaks in the growing season. However, the value and occurring time of the peaks varied with the precipitation and soil layer, and the seasonal variations of SMBC and SMBN in the 0-5 cm soil layer were higher than in the 5-10 cm soil layer. SMBC and SMBN had significant positive correlation with organic matter and total nitrogen content. The variances of soil physical and chemical properties caused by precipitation variation were closely related with the difference in spatial-temporal patterns of the soil microbial biomass in the forest. In conclusion, the precipitation variations could cause the change of the soil microbial community structure and composition.
阔叶红松混交林是中国东北地区的地带性顶级植被,在维护生态安全方面发挥着重要作用。长白山是研究温带森林对降水变化正负反馈机制的适宜区域。本研究分析了长白山原始阔叶红松混交林土壤微生物生物量碳(SMBC)和微生物生物量氮(SMBN)对降水变化(±30%)的响应。结果表明,在生长季节(5月至9月),SMBC和SMBN的平均值分别为879.09和100.03 mg·kg(-1)。此外,这两个参数均随土壤深度逐渐降低。SMBC和SMBN的含量均随降水量增加而增加,且0-5 cm土层中SMBC和SMBN的变化比5-10 cm土层更强。SMBC/SMBN值随降水量增加而下降。降水变化显著影响SMBC和SMBN的均值。与降水减少相比,降水增加对这些指标的影响更为显著。SMBC和SMBN均呈现相似的季节模式,5月最低,之后先升高后降低再升高,在生长季节出现1-2个峰值。然而,峰值的大小和出现时间随降水量和土层而异,0-5 cm土层中SMBC和SMBN的季节变化高于5-10 cm土层。SMBC和SMBN与有机质和全氮含量呈显著正相关。降水变化引起的土壤理化性质差异与森林土壤微生物生物量时空格局的差异密切相关。总之,降水变化会导致土壤微生物群落结构和组成的改变。