Mapping a Fluvial Aquifer in New Zealand Using Airborne Tem, Seismic, and Electrical Soundings

R. Kellett, Z. Rawlinson, R. Westerhoff, R. Reeves, J. Smith, S. Harper, N. Foged, J. Pedersen, P. Maurya
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Abstract

Summary A SkyTEM airborne survey has been flown over 1820 km2 of an area of intense agriculture in Hawkes Bay region of New Zealand. The survey is designed to map the characteristics of a coastal fluvial aquifer and support the management of groundwater resources. Processing the data from a 590 km2 subset of the survey, adjacent three urban centres, has been helped by using ground-based geophysical data. These data include ground-TEM, DC resistivity soundings, and borehole geophysical logs. Seismic reflection data across the region provide constraints on the deeper sections of the aquifer system (200 – 500 m). One of the key aims of the study is to map the variability of the surface geological strata that in places are a recharge zone and in other places a confining layer for the aquifer. The SkyTEM data have a spatial coverage (170 m line spacing and 20–30 m station spacing) that enables these units to be mapped in more detail than is possible with the current boreholes and ground geophysical data. In places the ground-based data provide valuable support for constraining the shallow SkyTEM models where data can be missing and deep parts of the SkyTEM model where the resolution is low.
利用机载Tem、地震和电测深测绘新西兰的河流含水层
SkyTEM对新西兰霍克斯湾地区1820平方公里的集约化农业区域进行了空中调查。这次调查的目的是绘制沿海河流含水层的特征图,并支持地下水资源的管理。利用地面地球物理数据有助于处理毗邻三个城市中心的590平方公里调查子集的数据。这些数据包括地面瞬变电磁法、直流电阻率测深和钻孔地球物理测井。整个地区的地震反射数据提供了含水层系统深层部分(200 - 500米)的约束条件。该研究的主要目的之一是绘制地表地质层的变异性图,地表地质层在某些地方是补给带,在其他地方是含水层的限制层。SkyTEM数据具有空间覆盖范围(线间距为170米,站间距为20-30米),与目前的钻孔和地面地球物理数据相比,可以更详细地绘制这些单元。在一些地方,地面数据提供了有价值的支持,以约束数据可能缺失的浅层SkyTEM模型和分辨率较低的SkyTEM模型的深层部分。
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