前锡矿池中磷、硫的分布及可培养细菌的时间序列

A. Kurniawan, O. Oedjijono, Tamad Tamad, U. Sulaeman
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引用次数: 2

摘要

锡矿开采造成了宏观生态系统和微观生态系统的生态变化。本文旨在研究锡矿池中磷、硫元素的分布规律,并对从锡矿池中分离出的可培养细菌进行时间序列鉴定。采用x射线荧光法(XRF)检测P、S元素,用培养基分离细菌,并用微生物进行生物化学鉴定。前锡矿池中磷元素和硫元素的浓度表现为磷元素的平均浓度随时间顺序增加,而硫元素的平均浓度则表现为动态变化。龄< 1年的前锡矿池中磷的平均浓度为33,725 mg。L-1和S分别为311和45 mg.L-1。前锡矿池5 ~ 10年的磷含量为59.8 mg.L-1, S含量为451 75 mg.L-1。年龄为bb0 ~ 15年的前锡矿池中P含量为67,44 mg.L-1, S含量为386,125 mg.L-1。可培养细菌为克氏菌;放线杆菌equuli;芽孢杆菌amyloliquefaciens;芽孢杆菌spp;微球菌sp;肠杆菌属gergoviae;韦永氏球菌属sp;肠杆菌属aerogenes;莫拉克斯氏菌属宝;Nitrobater spp;肠杆菌聚集。
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The Phosphorus and Sulphur Distribution and Culturable Bacterial In Time Chronosequence of Ex-Tin Mining Ponds
The tin mining had caused ecological changes that can be occured to macro- and microecosystem. This article aims to study the pattern distribution of element of phosphorus (P) and sulphur (S) and also to identify culturable bacterial that were isolated form ex-tin mining ponds in time chronosequence. The elemets of P and S were detected by X-Ray Fluorescence (XRF) and the bacterials was isolated in medium agar and biochemistry identification by microbact. The concentration of element of P and S showed the average of P concentration increased in time chronosequnce of ex-tin mining ponds, whereas the average of S concentration showed dynamic pattern. In ex-tin mining pond with age < 1 year the average concentration of P was 33,725 mg.L-1 and S was 311,45 mg.L-1. In ex-tin mining pond with age 5-10 years were P (59,8 mg.L-1) and S (451,75 mg.L-1). In ex-tin mining pond with age > 15 years were P (67,44 mg.L-1) and S (386,125 mg.L-1). While, the culturable bacterials were Kurthia spp; Actinobacillus equuli; Bacillus amyloliquefaciens; Bacillus spp; Micrococcus sp; Enterobacter gergoviae; Veillonella sp; Enterobacter aerogenes; Moraxella bovis; Nitrobater spp; and Enterobacter agglomerans.
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