Pignatello J J, Johnson L K, Martinson M M, Carlson R E, Crawford R L
Appl Environ Microbiol. 1985 Jul;50(1):127-32. doi: 10.1128/aem.50.1.127-132.1985.
Outdoor artificial streams were treated continuously with pentachlorophenol (PCP) for 88 days during the summer of 1983. The contributions of different stream compartments (microbial habitats) to microbial degradation of PCP were determined in a stream treated with 144 micrograms of PCP per liter. The 488-m long stream was composed of mud-bottomed pools alternating with gravel riffles. PCP loss in the stream attributable to microbial degradation after an adaptation period was in the range of 55 to 74%. Contributions to PCP loss were determined for rock surface (epilithic), macrophyte surface (epiphytic), sedimentary, and water column communities by measuring rates of PCP disappearance in stream water, containing ambient concentrations of PCP, in contact with representative compartmental samples. The specific capability, in units of micrograms of PCP per hour per square meter of stream cross-sectional area (macrophytes at maximum plant density, water column at mean depth, upper 10-cm layer of gravel), followed the order rock surface much greater than macrophytes greater than sediment approximately equal to water column. The compartmental contribution to total stream losses in units of grams per hour followed the same order, although the differences were smaller. The rate of PCP disappearance in the water column above sediment cores followed the order oxygen-rich greater than oxygen-poor approximately equal to anaerobic greater than sorption-only conditions. The large difference in specific capability between the rock surface and sediment compartments could be attributed to oxygen deficiency (because of chemical and biological oxygen demand) in the sediments. Free-floating and particle-attached organisms in the water column were important to PCP biodegradation.
1983年夏季,户外人工溪流连续88天用五氯苯酚(PCP)进行处理。在一条每升处理144微克PCP的溪流中,确定了不同溪流区域(微生物栖息地)对PCP微生物降解的贡献。这条488米长的溪流由底部为泥的水池和砾石浅滩交替组成。适应期后,溪流中因微生物降解导致的PCP损失在55%至74%之间。通过测量与代表性区域样本接触的、含有环境浓度PCP的溪流水体中PCP的消失速率,确定了岩石表面(附石性)、大型植物表面(附植性)、沉积和水柱群落对PCP损失的贡献。以每小时每平方米溪流横截面积的PCP微克数为单位的特定能力(大型植物处于最大植物密度、水柱处于平均深度、砾石上层10厘米层),顺序为岩石表面远大于大型植物大于沉积物约等于水柱。以每小时克数为单位的各区域对溪流总损失的贡献遵循相同顺序,尽管差异较小。沉积物核心上方水柱中PCP的消失速率顺序为富氧大于缺氧约等于厌氧大于仅吸附条件。岩石表面和沉积物区域之间特定能力的巨大差异可归因于沉积物中的缺氧(由于化学需氧量和生物需氧量)。水柱中的自由漂浮和附着颗粒的生物对PCP生物降解很重要。