3D hydrostratigraphic and hydraulic conductivity modelling using supervised machine learning

被引:10
作者
Tilahun, Tewodros [1 ]
Korus, Jesse [2 ]
机构
[1] Univ Nebraska Lincoln, Sch Nat Resources, 3310 Holdrege St, Lincoln, NE 68583 USA
[2] Univ Nebraska Lincoln, Sch Nat Resources, Conservat & Survey Div, 3310 Holdrege St, Lincoln, NE 68583 USA
来源
APPLIED COMPUTING AND GEOSCIENCES | 2023年 / 19卷
基金
美国农业部;
关键词
3D hydrostratigraphy; Hydraulic conductivity modeling; Airborne electromagnetics; Machine learning; AQUIFER SYSTEM; RANDOM FOREST; GEOSTATISTICAL INVERSION; ELECTRICAL-RESISTIVITY; SLUG TESTS; COMPLEX; ELECTROMAGNETICS; SIMULATION; NETWORKS; NEBRASKA;
D O I
10.1016/j.acags.2023.100122
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Accurately modeling highly heterogenous aquifers is one of the big challenges in hydrogeology. There is a pressing need to develop new methods that transform high-resolution data into hydrogeological parameters representative of such aquifers. We use random forest-based machine learning to predict the distribution of hydrostratigraphic units and hydraulic conductivity (K) at a regional scale. We used lithologic logs from >2000 boreholes and resistivity-depth models from 2717 km of Airborne Electromagnetics (AEM). Eighty unique lithologic categories are lumped into 5 hydrostratigraphic units. K data is derived from descriptions of grain size and texture. The input data are resampled into a 200 x 200 x 1m grid and split into 70% training and 30% validation. K prediction had a training F1 score of 95% and 87% testing accuracy. After hyperparameter tuning these scores improved to 99.6% and 92%, respectively. Hydrostratigraphic unit prediction showed a training F1 score of 97% and 91% testing accuracy, improving to 100% and 95% after hyperparameter tuning. This method produces a high-resolution 3D model of K and hydrostratigraphic units that fills gaps between widely spaced boreholes. It is applicable in any setting where boreholes and AEM are available and can be used to build robust groundwater models for heterogeneous aquifers.
引用
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页数:16
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