SGER: Microbial Alteration of Basaltic Glass in seawater: Feasibility Study on Loihi Seamount and the Flanks of Hawaii
SGER: Microbial Alteration of Basaltic Glass in seawater: Feasibility Study on Loihi Seamount and the Flanks of Hawaii
批准号:
0218945
负责人:
Hubertus Staudigel
金额:
$7.07万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2002
资助国家:
美国
项目状态:
已结题
起止时间:
2002-04-01 至 2003-03-31
中文摘要
PI将进行新鲜玄武岩玻璃在海底海水中的暴露实验,并将结果与同一地点暴露的天然玄武岩玻璃在微生物群落在玻璃变化中的作用进行比较。研究环境位于夏威夷的海底斜坡上,水深200-2000米,水温从接近冰点到大约80摄氏度的热泉温度。裸露的岩石表面的年龄从几年到几个100公里不等,包括洛伊希海山、普纳岭和科哈拉和华莱的海底斜坡。利用NOAA NURP计划的其他资金,PIS将在2002/2003财年进行16次潜水,以进行实地部分的研究。这一奖励将支持邮轮参与收回先前提出的暴露费用,以及对潜水中找到的材料进行化学和微生物实验室调查。PIS将观察和表征玻璃表面上自然微生物变化的微生物种群和物理影响。他们将比较一年暴露实验中的反应速率与几年到近一百万年自然暴露中玄武岩的变化速率。化学质量平衡将使PI能够确定海水和玄武岩暴露实验之间的化学交换率。
英文摘要
The PI will carry out exposure experiments of fresh basaltic glass in seawater on the ocean floor, and compare the results to the behavior of natural basalt glass exposed at the same site in terms of the role of microbial communities in the alteration of the glass. Study environments are located on the submarine slopes of Hawaii at water depths ranging from 200-2000m, at water temperatures ranging from near freezing to hydrothermal spring temperatures of approximately 80 degree C. Exposed rock surfaces vary in age from a few years to several 100kyrs and include sites on Loihi Seamount, Puna Ridge and the submarine slopes of Kohala and Hualalai. With other funds from NOAA's NURP program, the PIs will undertake 16 submersible dives in FY's 2002/2003, to carry out the field portion of the study. This award will support cruise participation for the recovery of previously-placed exposure charges, and the chemical, and microbiological laboratory investigations of materials recovered from the dives. The PIs will observe and characterize the microbial populations and physical effects of natural microbial alteration on well defined glass surfaces. They will compare reaction rates in the one-year exposure experiments to the rates of basalt alteration in natural exposure of several years to nearly a million years. Chemical mass balance will allow the PIs to determine the chemical exchange rates between seawater and the basalt exposure experiments.
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