黄土丘陵区不同坡向对土壤微生物生物量和可溶性有机碳的影响

选取黄土高原丘陵沟壑区延河流域两个典型植被区(森林植被区、草原植被区)下相同植被不同坡向(阳坡、阴坡)的土样进行分析,研究了不同坡向土壤微生物生物量碳(SMBC)、微生物生物量氮(SMBN)、微生物生物量磷(SMBP)和可溶性有机碳(DOC)的含量及其相互关系.结果表明,森林植被区阳坡、阴坡0～10 cm土层SMBC分别为532.1～792.5 mg·kg-1、333.6～469.8 mg·kg-1,SMBN分别为53.66～87.31 mg·kg-1、47.58～61.38 mg·kg-1,两者均表现为阳坡高于阴坡,草原植被区SMBC分别为68.90～75.34 mg·kg-1、65.29～128.67 mg·kg-1,SMBN分别为13.94～18.61 mg·kg-1、13.00～20.10mg·kg-1,两者均表现为阴坡高于阳坡;两个植被区SMBP与SMBC、SMBN变化不一致;SMBC占SMBC与DOC之和(SMBC+DOC)的比例在森林植被区阳坡最高,达77.74%,在草原植被区按阴坡到阳坡、0～10 cm土层到10～30 cm土层的顺序依次递减.相同植被区不同坡向土壤水分、温度的差异对土壤微生物生物量产生重要影响,进而使SMBC占SMBC+DOC的比例不同,SMBC+DOC比SMBC更能反映土壤碳素有效性,森林植被区阴坡阳坡0～10 cm土层土壤微生物群落结构可能已发生明显改变.

Effects of Different Aspects on Soil Microbial Biomass and Dissolved Organic Carbon of the Loess Hilly Area

Soil samples from different aspects(southern slope and northern slope) under the same vegetation in two typical vegetation zones(forest vegetation zone and steppe vegetation zone) of Yanhe basin in the loess hilly area were chosen and analyzed, in order to investigate the content and correlation of soil microbial biomass carbon (SMBC), soil microbial biomass nitrogen (SMBN), soil microbial biomass phosphorus (SMBP) and dissolved organic carbon (DOC). The results show that, in 0-10 cm soil layer of forest vegetation zone, SMBC in southern slope and northern slope are 532.1-792.5 mg·kg^-1 and 333.6-469.8 mg·kg^-1, SMBN are 53.66-87.31 mg·kg^-1 and 47.58-61.38 mg·kg^-1 respectively, both of them are higher in southern slope than those in northern slope, but in steppe vegetation zone, SMBC and SMBN in southern slope are lower than those in northern slope, with SMBC of southern slope and northern slope are 68.90-75.34 mg·kg^-1 and 65.29-128.67 mg·kg^-1, SMBN are 13.94-18.61 mg·kg^-1 and 13.00-20.10 mg·kg^-1 respectively, SMBP in both vegetation zones have a different variation trend compared with SMBC and SMBN; the ratio of SMBC to the sum of SMBC plus DOC(SMBC+DOC) in southern slope of forest vegetation zone reaches the maximum value in two vegetation zones, which is 77.74%. In steppe vegetation zone, this ratio both decreases from northern slope to southern slope and 0-10 cm soil layer to 10-30 cm soil layer. The difference of soil moisture and temperature between different aspects under the same vegetation have a significant effect on soil microbial biomass, it also makes the ratio of SMBC to SMBC+DOC different, SMBC+DOC can reflect soil carbon availability better than SMBC, there might be an obvious change in soil microbial communities in 0-10 cm soil layer of different aspects in forest vegetation zone.