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Natural organic matter (NOM) removal and structural changes in the bacterial community during artificial groundwater recharge with humic lake water

机译:腐殖质湖水人工补给地下水过程中天然有机物(NOM)的去除和细菌群落的结构变化

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This study evaluated the removal of natural organic matter (NOM) and structural changes in the rnicrobial community during infiltration of humic lake water at three artificial groundwater recharge (AGR) sites in Finland. The three sites were at waterworks in Haemeenlinna, Jyvaeskylae and Tuusula, sites A, B and C, respectively. Site A used ground-water recharge by both basin and sprinkling infiltration, site B used only sprinkling infiltration, and site C used only basin infiltration. Reductions of total organic carbon at sites A, B and C were 91%, 84% and 74%, respectively, in the winter, and 88%, 77% and 73%, respectively, in the summer. The Finnish national recommended value of 2 mg/l for TOC was achieved at all sites and the TOC of natural groundwater at site C was much lower, at 0.6 mg/l. Large molecular fractions of NOM were removed more efficiently than the smaller ones. Total amount of DAPI-stained cells decreased during infiltration at sites A, B and C in winter by 94%, 94% and 75% and in summer by 96%, 97% and 94%, respectively. Bacterial communities in raw waters and extracted groundwaters were diverse with changes occurring during infiltration, which was shown by DNA extraction followed by PCR of 16S rRNA genes and denaturing gradient gel electrophoresis (DGGE) fingerprinting. While the natural groundwater rnicrobial community was diverse, it was different from that of the extracted groundwater in the AGR area. Simultaneous organic carbon removal and the decrease of bacterial counts during infiltration indicated biodegradation. In addition, the changing DGGE profiles during the process of infiltration, demonstrated that changing environmental conditions were reflected by changes in bacterial community composition.
机译:这项研究评估了在芬兰三个人工地下水补给(AGR)地点腐殖质湖水渗透过程中,尼克有机体的去除和菱形群落的结构变化。这三个地点分别在Haemeenlinna,Jyvaeskylae和Tuusula的自来水厂,地点A,B和C。地点A通过盆地和洒水入渗利用地下水补给,地点B仅用于洒水入渗,而地点C仅用于水池入渗。冬季,地点A,B和C的总有机碳减少量分别为91%,84%和74%,夏季分别为88%,77%和73%。在所有地点,芬兰国家对TOC的推荐值均达到2 mg / l,而在C点,天然地下水的TOC则低得多,为0.6 mg / l。 NOM的大分子部分比较小的部分更有效地被去除。在冬季,分别在A,B和C地点渗透的DAPI染色的细胞总数分别减少了94%,94%和75%,夏季减少了96%,97%和94%。原水和提取的地下水中的细菌群落是多种多样的,并在渗透过程中发生变化,这通过DNA提取,16S rRNA基因的PCR和变性梯度凝胶电泳(DGGE)指纹图谱显示。尽管天然的地下尼克类菌群落种类繁多,但与AGR地区提取的地下水有所不同。渗透过程中同时去除有机碳和减少细菌计数表明生物降解。此外,渗透过程中DGGE分布的变化表明细菌群落组成的变化反映了环境条件的变化。

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