[1]FAN Yuanyuan,LI Yi,LI Qidi.Microbe, Enzymatic Activity and Nutrient Contents of Soils in Different Stand Ages of Pinus tabuliformis[J].Research of Soil and Water Conservation,2019,26(06):58-64.
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Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
26
Number of periods:
2019 06
Page number:
58-64
Column:
Public date:
2019-10-17
- Title:
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Microbe, Enzymatic Activity and Nutrient Contents of Soils in Different Stand Ages of Pinus tabuliformis
- Author(s):
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FAN Yuanyuan1, LI Yi2, LI Qidi3
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1. Shandong Normal University, Jinan, Shandong 250100, China;
2. Aba Teachers College, Wenchuan, Sichuan 623002, China;
3. Shandong Vocational College of Biology, Jinan, Shandong 250100, China
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- Keywords:
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Pinus tabuliformis; soil nutrients; soil enzyme activity; soil microbial diversity
- CLC:
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Q154
- DOI:
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- Abstract:
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We studied the soil microbe, enzyme activity and nutrients of soil in the rhizosphere and non-rhizosphere in different stand ages of Pinus tabuliformis in Minjiang River valley. The results showed that:(1) the soil pH of Pinus tabulata was slight acidity, and the organic carbon contents in the rhizosphere and non-rhizosphere showed a trend of decreasing and then increasing with the increase of ages of Pinus tabulata, and reached the lowest at the mature stage; the pH of the rhizosphere soil in different growth stages was significantly lower than that in the non-rhizosphere soil (p<0.05); (2) in the rhizosphere and non-rhizosphere, the contents of soil organic carbon, total nitrogen, available phosphorus and available potassium presented the consistent with the trend which showed the increase at first, and then the decrease, and reached up to the peak values in the mature forest stage with the increase of the ages of Pinus tabulaeformis, rhizosphere the contents of organic carbon, total nitrogen, available phosphorus and available potassium in the rhizosphere of young forest, middle forest and mature forest were significantly higher than those of the non-rhizosphere (p<0.05), the contents of soil organic carbon, total nitrogen, available phosphorus and available potassium in the rhizosphere of the aged forest were not significant difference from those of the non-rhizosphere (p>0.05); (3) soil enzyme activities (sucrase activity, the activity of alkaline phosphatase, urease activity and catalase activity) and microbial community diversity, species richness index, evenness index, dominance index, carbon source utilization index) in the rhizosphere and non-hizosphere were consistent with the trend which showed the increase at first, and then the decrease, reached up to the peak values in the mature forest stage, soil enzyme activities and microbial community diversity in rhizosphere of young forest, middle forest and mature forest were significantly higher than those of the non-rhizosphere (p<0.05), there was no significant difference in enzyme activity and microbial community diversity between rhizosphere soil and non-rhizosphere soil of the aged forest (p>0.05); (4) because of the influence of microbial community on slightly rhizospheric secretion, the microbe amounts of Pinus tabulaeformis rhizosphere were higher than those of the non-rhizosphere, the proportion of bacteria to the total microbe in the rhizosphere and non-rhizosphere was the highest, the proportion of actinomycete to the total microbe in the rhizosphere and non-rhizosphere was the least; (5) correlation analysis showed that there was a negative correlation between the functional diversity of soil microbial community and soil pH, which was significantly correlated with soil organic carbon and total nitrogen, sucrase activity, alkaline phosphatase activity, number of bacteria and total number of microorganisms; therefore, soil pH negatively contributed to soil microbial community functional diversity, and soil nutrient, soil enzyme activity and microbial quantity had the positive contribution to soil microbial community functional diversity, soil organic carbon and total nitrogen, invertase activity, alkaline phosphatase activity, number of bacteria and the total number of microorganisms are the main influence factors on the soil microbial community diversity.