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首页> 外文期刊>Geophysical Research Letters >Location for direct access to subglacial Lake Ellsworth: An assessment of geophysical data and modeling
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Location for direct access to subglacial Lake Ellsworth: An assessment of geophysical data and modeling

机译:直接进入冰河以下埃尔斯沃思湖的位置:地球物理数据和模型评估

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摘要

Subglacial Lake Ellsworth has been proposed as a candidate for direct measurement and sampling, to identify microbial life and extract sedimentary climate records. We present a detailed characterization of the physiography of this subglacial lake from geophysical surveys, allowing bathymetry and geomorphic setting to be established. Lake Ellsworth is 14.7 km × 3.1 km with an area of 28.9 km~2. Lake depth increases downlake from 52 m to 156 m, with a water body volume of 1.37 km~3. The ice thickness suggests an unusual thermodynamic characteristic, with the critical pressure boundary intersecting the lake. Numerical modeling of water circulation has allowed accretion of basal ice to be estimated. We collate this physiographic and modeling information to confirm that Lake Ellsworth is ideal for direct access and propose an optimal drill site. The likelihood of dissolved gas exchange between the lake and the borehole is also assessed.
机译:已建议将冰河以下埃尔斯沃思湖作为直接测量和取样的候选者,以鉴定微生物生命并提取沉积气候记录。我们从地球物理调查中对该冰川下湖泊的生理特征进行了详细描述,从而可以建立测深法和地貌环境。埃尔斯沃思湖是14.7公里×3.1公里,面积28.9公里〜2。湖泊深度使下湖从52 m增加到156 m,水体体积为1.37 km〜3。冰的厚度暗示了不寻常的热力学特征,临界压力边界与湖泊相交。水循环的数值模型可以估算基础冰的积聚。我们整理这些地貌和模型信息,以确认埃尔斯沃思湖是直接通道的理想选择,并提出了一个最佳的钻探地点。还评估了湖泊和钻孔之间溶解气体交换的可能性。

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