Grant I F, Bancroft K, Alexander M
Appl Environ Microbiol. 1979 Jul;38(1):78-83. doi: 10.1128/aem.38.1.78-83.1979.
Glucose oxidation was inhibited in a forest soil (pH 4.01) previously exposed by 1.0 microliter of SO2 per liter, the extent of inhibition and the decline in pH being directly related to the length of exposure. The phase of rapid CO2 evolution in protein hydrolysate-amended soil previously treated with 5.0 microliter of SO2 per liter for 24 h or 1.0 microliter/liter for 48 h was delayed, but the degradation of the amino acid mixture then proceeded rapidly. Bacterial numbers in soil incubated for 48 h with 1.0 microliter of SO2 per liter were reduced, but the bacteria grew rapidly if glucose or an amino acid mixture was added after the exposure period. Low levels of bisulfite inhibited amino acid decomposition in soil at pH 3.89, but the effect was less pronounced in soil at pH 4.01. Comparable levels of sulfate were not toxic to carbon mineralization. Approximately 1.0 microgram of bisulfite S and about 20 microgram of sulfate S per g of soil appeared when the soil was treated with 1.0 microliter of SO2 per liter for 48 h. Bisulfite added to the soil disappeared readily. The possible ecological significance of the findings is discussed.
在先前每升暴露于1.0微升二氧化硫的森林土壤(pH 4.01)中,葡萄糖氧化受到抑制,抑制程度和pH值下降与暴露时间直接相关。在先前每升用5.0微升二氧化硫处理24小时或每升1.0微升处理48小时的蛋白质水解物改良土壤中,快速释放二氧化碳的阶段被延迟,但随后氨基酸混合物的降解迅速进行。每升用1.0微升二氧化硫培养48小时的土壤中细菌数量减少,但如果在暴露期后添加葡萄糖或氨基酸混合物,细菌会迅速生长。低水平的亚硫酸氢盐在pH 3.89的土壤中抑制氨基酸分解,但在pH 4.01的土壤中这种作用不太明显。相当水平的硫酸盐对碳矿化无毒。当土壤每升用1.0微升二氧化硫处理48小时时,每克土壤中出现约1.0微克亚硫酸氢盐硫和约20微克硫酸盐硫。添加到土壤中的亚硫酸氢盐很容易消失。讨论了这些发现可能的生态意义。