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Huanjing Kexue/Environmental Science 2015-May

[Soil Microorganism Characteristics and Soil Nutrients of Different Wetlands in Sanjinag Plain, Northeast China].

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پیوند در کلیپ بورد ذخیره می شود
Ye Xiao
Zhi-gang Huang
Hai-tao Wu
Xian-guo Lü

کلید واژه ها

خلاصه

Four typical wetland types (i.e. wetlands with the following dominant plant species: Calamagrostis angustifolia + Salix brachypoda, Calamagrostis angustifolia, Carex lasiocarpa and Phragmites australis) of the Honghe reserve in Sanjiang Plain were studied to investigate the distribution of soil microorganism quantity and enzyme activity and their relationships with soil nutrients. The results showed that in 0-30 cm soil layer of these four wetlands: (1) Contents of soil total organic carbon, total nitrogen and total phosphorus decreased with the increase of soil depth, while available nitrogen, phosphorus and potassium did not exhibit regularly changes. Moreover, there were significantly different for soil nutrient contents among different wetland types (P < 0.05). (2) The number of soil microorganism was bacteria > actinomycetes > fungi, furthermore, the number of three microbial colonies all decreased with the increase of soil depth. Total soil microbial number of C. angustifolia wetland was the highest and that of C. lasiocarpa wetland was the lowest. (3) Soil invertase and cellulase activities decreased with soil depth, while soil catalase activity showed no consistent changes. Three kinds of enzyme activities in C. angustifolia + S. brachypoda and C. angustifolia wetlands were significantly higher than those of C. lasiocarpa and P. australis wetlands (P < 0.05). (4) The correlation analysis showed that soil bacteria, fungi and cellulose activity had a significant correlation with indicators of soil nutrients. But there was no correlation between actinomyces, invertase and available potassium, as well as between catalase and available potassium, available phosphorus. Overall, soil microorganism and enzyme activities are important indicators for reflecting the status of soil nutrients.

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