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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Percolation flux and transport velocity in the unsaturated zone, Yucca Mountain, Nevada
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Percolation flux and transport velocity in the unsaturated zone, Yucca Mountain, Nevada

机译:内华达州尤卡山非饱和带的渗流通量和传输速度

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摘要

The percolation flux for borehole USW UZ-14 was calculated from C-14 residence times of pore water and water content of cores measured in the laboratory. Transport velocity is calculated from the depth interval between two points divided by the difference in C-14 residence times. Two methods were used to calculate the flux and velocity. The first method uses the 14C data and cumulative water content data directly in the incremental intervals in the Paintbrush nonwelded unit and the Topopah Spring welded unit. The second method uses the regression relation for 14C data and cumulative water content data for the entire Paintbrush nonwelded unit and the Topopah Spring Tuff/Topopah Spring welded unit. Using the first method, for the Paintbrush nonwelded unit in borehole USW UZ-14 percolation flux ranges from 2.3 to 41.0 mm/a. Transport velocity ranges from 1.2 to 40.6 cm/a. For the Topopah Spring welded unit percolation flux ranges from 0.9 to 5.8 mm/a in the 8 incremental intervals calculated. Transport velocity ranges from 1.4 to 7.3 cm/a in the 8 incremental intervals. Using the second method, average percolation flux in the Paintbrush nonwelded unit for 6 boreholes ranges from 0.9 to 4.0 mm/a at the 95% confidence level. Average transport velocity ranges from 0.6 to 2.6 cm/a. For the Topopah Spring welded unit and Topopah Spring Tuff, average percolation flux in 5 boreholes ranges from 1.3 to 3.2 mm/a. Average transport velocity ranges from 1.6 to 4.0 cm/a. Both the average percolation flux and average transport velocity in the PTn are smaller than in the TS/TSw. However, the average minimum and average maximum values for the percolation flux in the TS/TSw are within the PTn average range. Therefore, differences in the percolation flux in the two units are not significant. On the other hand, average, average minimum, and average maximum transport velocities in the TS/TSw unit are all larger than the PTn values, implying a larger transport velocity for the TS/TSw although there is a small overlap. Published by Elsevier Science Ltd. [References: 18]
机译:根据实验室测量的孔隙水的C-14停留时间和岩心含水量计算出井壁USW UZ-14的渗流通量。传输速度由两点之间的深度间隔除以C-14停留时间之差得出。使用两种方法来计算通量和速度。第一种方法直接在画笔非焊接单元和​​Topopah Spring焊接单元中以递增间隔使用14C数据和累积水含量数据。第二种方法使用14C数据的回归关系和整个画笔非焊接单元和​​Topopah Spring Tuff / Topopah Spring焊接单元的累积水含量数据。使用第一种方法,对于井壁USW UZ-14中的画笔非焊接单元,渗透通量范围为2.3至41.0 mm / a。输送速度为1.2至40.6 cm / a。对于Topopah Spring,在计算的8个增量间隔中,渗流通量范围为0.9至5.8 mm / a。在8个增量间隔中,传输速度范围为1.4至7.3 cm / a。使用第二种方法,在95%置信度下,画笔的6个非焊接单元的平均渗透通量在0.9到4.0 mm / a的范围内。平均输送速度为0.6至2.6 cm / a。对于Topopah Spring焊接单元和​​Topopah Spring Tuff,在5个钻孔中的平均渗透通量范围为1.3至3.2 mm / a。平均输送速度为1.6至4.0 cm / a。 PTn中的平均渗透通量和平均传输速度均小于TS / TSw。但是,TS / TSw中的渗透通量的平均最小值和平均值在PTn平均值范围内。因此,两个单元中的渗透通量的差异并不显着。另一方面,TS / TSw单位中的平均,平均最小和最大平均运输速度都大于PTn值,这意味着TS / TSw的运输速度较大,尽管重叠很小。由Elsevier Science Ltd.发布[参考文献:18]

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