Kinetically Activated Subsurface Micribial Sampler (KASMS)

地震及其余震以地震波、热量、应变、岩石破裂和产生氢气的化学反应的形式产生能量。地震活动产生的重复能量脉冲能刺激产生甲烷和醋酸的地下生命吗？这种微生物活动是否影响余震的频率和分布？2017年，国际大陆钻探计划(ICDP)支持的DSEIS(钻探孕震区)项目将研究导致2014年奥克尼5.5级地震的一个以前不为人知的断裂带，这是南非50多年来最大的地震。在Moab KhotSong金矿底部3公里深的地方，地球物理学家和地球微生物学家将联手向下钻入这一仍在活动的断裂带600米，分析岩心样品，安装地震仪器，并部署动态激活地下微生物采样器(KASMS)。KASMS是一种新型的、便携式的、自主的流体采样和保存设备，它将在断裂带的地震事件中触发。这项研究的数据将大大提高我们对与超深采矿、水力压裂和水力压裂卤水注入相关的地震类型的了解，从而更好地为安全和环境法规提供信息。高分辨率的时间数据将提供地下微生物群落如何对环境刺激(如氢气脉冲)做出反应的第一张图片。如果在断裂带内发现了实质性的生物量增强，那么暴露在火星表面的类似的古老断裂带可能会被选为火星2020漫游车任务的第一步，这是火星样本返回任务系列的第一步。在来自日本、南非、瑞士、以色列、德国、印度、澳大利亚和美国的地球物理、地质学、岩石力学和地球微生物学学生的参与下，DSEIS和这个项目将促进跨学科的国际STEM教育。通过取芯和采样活动的视频以及KASMS的安装和操作视频，以及井下视频，DSEIS和这个项目将向公众介绍科学是如何在地球上最极端的环境之一进行的，以及地下生命对地球和可能其他行星上生命的起源和进化说了什么。这个为期两年的项目将设计、建造和部署KASMS，这是第一个用于地球化学和微生物研究的全自动采样设备。KASMS由井下部署的U型管流体采样系统和用于监测井筒环境的离散传感器阵列组成。KASMS还将包含两个渗透采样器和矿物券，以收集断层带内的生物膜。KASMS系统的独特之处在于能够自主响应地震事件并捕获流体样本的时间进程。这些样品将进行水化学、溶解气体浓度和同位素值分析，并将使用两种带有防腐剂的过滤器进行亚采样，一种用于扫描电子显微镜，另一种用于后基因组/后转录/后蛋白质组分析。在Moab KhotSong金矿部署KASMS的这一年里，将进行正负对照试验：在断裂带内发生小规模地震事件之前和之后，在矿井爆炸之前、期间和之后，在矿山不活跃的采矿假期期间，以及在注入氢气和甲烷气体之前、期间和之后采集样本。一年后，KASMS将被取回并送回普林斯顿大学，在那里它将可用于部署到其他地下微生物站点。

Earthquakes and their after shocks generate energy in the form of seismic waves, heat, strain, fractured rock and chemical reactions producing hydrogen gas. Can the repeated energy pulses from seismic activity stimulate subsurface life that generates methane and acetic acid? Does this microbial activity impact the frequency and distribution of after shocks? In 2017 the International Continental Drilling Program (ICDP) supported DSeis (Drilling into Seismogenic Zones) project will examine a previously unknown fault zone responsible for the 2014 5.5-magnitude Orkney earthquake, South Africa's largest earthquake in over 50 years. At a depth of 3 km in the bottom of Moab Khotsong gold mine, geophysicists and geomicrobiologists will join forces to drill down an additional 600 meters into this still-active fault zone, analyze core samples, install seismic instruments and deploy a Kinetically Activated Subsurface Microbial Sampler (KASMS). KASMS is a novel, portable, autonomous fluid sampling and preservation device that will be triggered by seismic events along the fault zone. The data from this study will significantly advance our understanding of the type of earthquakes that are associated with ultra-deep mining, hydrofracking and fracking brine injections and thus better inform safety and environmental regulations. The high-resolution temporal data will provide the first picture of how subsurface microbial communities respond to environmental stimuli, such as hydrogen gas pulses. If a substantial biomass enhancement is found within the fault zone, then similar ancient fault zones exposed on the surface of Mars may be selected for the Mars 2020 rover mission, the first step in the Mars Sample Return mission series. With the involvement of geophysics, geology, rock mechanics, and geomicrobiology students from Japan, South Africa, Switzerland, Israel, Germany, India, Australia and the United States, DSeis and this project will stimulate cross-disciplinary international STEM education. Through videos of the coring and sampling activity and of the installation and operation of KASMS, and downhole videos of the borehole, DSeis and this project will relate to the public how science is conducted in one of the most extreme environments on the planet and what subsurface life says about the origin and evolution of life on Earth and possibly other planets. This two-year project will design, construct and deploy KASMS, the first fully automated sampling device for geochemical and microbiological studies. KASMS is comprised of a borehole-deployed U-tube fluid sampling system and a discrete sensor array for monitoring the wellbore environment. KASMS will also contain two osmo-samplers combined with mineral coupons to collect biofilms within the fault zone. Unique to the KASMS system is the capability to autonomously respond to seismic events and capture a time progression of fluid samples. These samples will be analyzed for aqueous geochemistry, dissolved gas concentrations and isotopic values, and they will be subsampled using two types of filters with preservatives, one for SEM/TEM microscopy and the other for metagenomic/metatranscriptomic/metaproteomic analyses. During the year that KASMS is deployed at Moab Khotsong gold mine, experiments will be performed with positive and negative controls: samples collected before and after small magnitude seismic events within the fault zone, before, during and after mine detonations, during mining holidays when the mine is inactive and before, during and after the injection of hydrogen and methane gas. After one year KASMS will be retrieved and returned to Princeton University, where it will be available for deployment to other subsurface microbiology sites.