频域电磁数据和直流电阻数据的地理统计联合反转用于近地表建模
João Narciso1, Jeroen Verhegge2, Ellen Van De Vijver2
1Department of Energy and Mineral Resources Engineering, CERENA, Instituto Superior Técnico, Universidade de Lisboa, Lisboa, Portugal. joao.narciso@tecnico.ulisboa.pt.
这项研究引入了一种新的地理统计联合倒置方法,将电电阻断层扫描 (ERT) 和频域电磁感应 (FDEM) 整合起来. 该方法提高了近地表面环境中小规模地下异质性的准确成像.
科学领域:
- 地质物理学 地质物理学
- 接近地表的探索探索.
- 地质统计学 在地质统计学
背景情况:
- 像ERT和FDEM这样的地球物理方法对于近地表面成像至关重要.
- 地下电导率 (EC) 估计依赖于数据逆转.
- 由于分辨率和非线性差异,ERT和FDEM数据的联合反转具有挑战性.
研究的目的:
- 为整合FDEM和ERT数据开发一种代的地理统计联合反转方法.
- 提高近地表面环境中小规模空间异质性建模的准确性.
- 通过使用地理统计学模拟和共模拟来克服联合倒置的挑战.
主要方法:
- 代地缘统计联合反转.
- 集成频域电磁 (FDEM) 和电电阻断层扫描 (ERT) 数据.
- 地理统计模拟和共模拟的应用,用于模型更新.
主要成果:
- 联合倒置方法成功地改善了小规模异质性的解决.
- 地下模型的不确定性减少了,特别是在深度.
- 该方法在合成和现实世界的应用中都胜过了单个倒置技术.
结论:
- 拟议的地理统计联合反转方法有效地整合了FDEM和ERT数据.
- 这种方法提高了复杂的近地表面环境的特征.
- 它提供了一种更准确,更可靠的替代方案,而不是单个地质物理数据的反转.
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