Table 2 Statistical characteristics of source parameters, best objective function values, and iterations to convergence for different ensemble sizes across 30 EKI realizations.

From: Regularized ensemble Kalman inversion for robust and efficient gravity data modeling to identify mineral and ore deposits

Ensemble

size (Ne)

Best parameter estimations (median ± interquartile range) across 30 realizations

\(\:{A}\:\left(\:{m}{G}{a}{l}.{{m}}^{2}\:\right)\)

z (m)

\(\:{x}_{0}\) (m)

q

\(\:{\upmu\:}\)

Best

Obj (mGal)

Iterations to

convergence

50

528.39 ± 106.6

24.96 ± 0.15

-50.00 ± 0.00

0.99 ± 0.00

0.97 ± 0.05

2.7e-03 ± 0.01

407 ± 826

100

544.29 ± 61.3

24.99 ± 0.08

-49.99 ± 0.00

0.99 ± 0.00

0.97 ± 0.03

4.16e-04 ± 0.0

315 ± 453

150

598.65 ± 90.2

24.99 ± 0.00

-50.00 ± 0.00

1.00 ± 0.00

0.94 ± 0.04

4.06e-04 ± 0.0

262 ± 232

200

558.20 ± 116.6

25.00 ± 0.00

-50.00 ± 0.00

1.00 ± 0.00

0.96 ± 0.06

1.95e-04 ± 0.0

235 ±241

300

557.74 ± 111.6

24.99 ± 0.00

-49.99 ± 0.00

1.00 ± 0.00

0.96 ± 0.06

6.17e-05 ± 0.0

176 ± 85

400

557.81± 92.93

24.99 ± 0.00

-50.00 ± 0.00

1.00 ± 0.00

0.95 ± 0.05

7.94e-05 ± 0.0

190 ± 93

500

584.79 ± 98.8

25.00 ± 0.00

-50.00 ± 0.00

1.00 ± 0.00

0.95 ± 0.05

1.22e-04 ± 0.0

128 ± 75

True

500

25

-50

1

1

-

-