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首页> 外文期刊>日本土壤肥料学雑誌 >Relationships between the amount of microbial biomass and the physicochemical properties of soil - comparison between volcanic and non-volcanic ash soils.
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Relationships between the amount of microbial biomass and the physicochemical properties of soil - comparison between volcanic and non-volcanic ash soils.

机译:微生物生物量与土壤理化特性之间的关系-火山灰和非火山灰土壤的比较。

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摘要

The microbial biomass and some physicochemical properties of 9 volcanic ash soils and 7 non-volcanic ash soils in Japan were measured and their relationships analysed. The results showed: (1) the amounts of biomass C and N did not significantly differ between the volcanic (58-1504 mg C/kg, 10-180 mg N/kg) and non-volcanic ash soils (11-1118 mg C/kg, 2-124 mg N/kg); (2) in both soils, the amounts of biomass C and N showed significant relationships (r ?0.826, n = 7) with organic C content, total N content, total humus content, NaOH-extracted humic acid content, NaOH-extracted fulvic acid content and Al2O3 content. The relationships between the amounts of biomass C and N and the CEC and phosphate absorption coefficient were significant (r ?0.809, n= 9) only in volcanic ash soils, and the relationship between the amount of biomass and clay content was significant (r ?0.839, n = 7) in non-volcanic ash soils. The soil characteristics having significant relationships (r ?0.902, n = 9) with the amount of biomass also showed significant relationships (r ?0.827, n = 7) with fulvic acids, total humus, humic acids or organic C contents; and (3) the relationships between the amounts of biomass C and N and several soil characteristics such as organic C,total N, total humus, fulvic acids, humic acid content, CEC, phosphate absorption coefficient and Al2O3 content can be separated into the volcanic ash soil group and the non-volcanic ash soil group.
机译:测量了日本9个火山灰土壤和7个非火山灰土壤的微生物量和一些理化性质,并分析了它们之间的关系。结果表明:(1)火山(58-1504 mg C / kg,10-180 mg N / kg)和非火山灰土(11-1118 mg C)之间的生物量碳和氮含量没有显着差异。 / kg,2-124 mg N / kg); (2)在两种土壤中,生物量碳和氮的含量均与有机碳含量,总氮含量,总腐殖质含量,NaOH提取的腐殖酸含量,NaOH提取的腐殖质呈显着关系(r = 0.826,n = 7)。酸含量和Al2O3含量。仅在火山灰土壤中,生物量碳和氮的量与CEC和磷酸盐吸收系数之间的关系才显着(r = 0.809,n = 9),生物量和黏土含量的关系也很显着(r = 0.89,n = 9)。 0.839,n = 7)在非火山灰土壤中。与生物量有显着关系(r = 0.902,n = 9)的土壤特性也与黄腐酸,总腐殖质,腐殖酸或有机碳含量具有显着关系(r = 0.827,n = 7)。 (3)生物量碳,氮的含量与土壤某些有机碳,总氮,腐殖酸,富里酸,腐殖酸含量,CEC,磷酸盐吸收系数和Al2O3含量之间的关系可以分为火山灰土组和非火山灰土组。

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