Applied Geosciences - Geohydromodelling

Publications

Hu, L., Doetsch, J., Brauchler, R., & Bayer, P. (2017). Characterizing CO2 plumes in deep saline formations: comparison and joint evaluation of time-lapse pressure and seismic tomography. Geophysics, 82(4), ID1-ID18, Available at: https://doi.org/10.1190/geo2016-0365.1

Hu, L., Bayer, P., & Brauchler, R. (2016). Detection of carbon dioxide leakage during injection in deep saline formations by pressure tomography. Water Resources Research52, 5676–5686, doi:10.1002/2015WR018420. Available at: http://onlinelibrary.wiley.com/doi/10.1002/2015WR018420/full

Hu, L., Bayer, P., Alt-Epping, P., Tatomir, A., Sauter, M., & Brauchler, R. (2015). Time-lapse pressure tomography for characterizing CO2 plume evolution in a deep saline aquifer. International Journal of Greenhouse Gas Control, 39, 91-106, doi: 10.1016/j.ijggc.2015.04.013. Available at: http://www.sciencedirect.com/science/article/pii/S1750583615001565

Jiménez, S., Brauchler, R., Hu, R., Hu, L., Schmidt, S., Ptak, T., & Bayer, P. (2015). Prediction of solute transport in a heterogeneous aquifer utilizing hydraulic conductivity and specific storage tomograms. Water Resources Research, 51, 5504-5520, doi: 10.1002/2014WR016402. Available at: http://onlinelibrary.wiley.com/doi/10.1002/2014WR016402/epdf

Brauchler, R., Hu, R., Hu, L., Jiménez, S., Bayer, P., Dietrich, P., & Ptak, T. (2013). Rapid field application of hydraulic tomography for resolving aquifer heterogeneity in unconsolidated sediments. Water Resources Research, 49, 2013-2024, doi: 10.1002/wrcr.20181. Available at: http://onlinelibrary.wiley.com/doi/10.1002/wrcr.20181/epdf

Brauchler, R., Hu, R., Hu, L., & Ptak, T. (2012). Bestimmung von hydraulischen Parametern in Lockergesteinen: Ein Vergleich unterschiedlicher Feldmethoden. Grundwasser, 17, 57-67, doi:10.1007/s00767-011-0185-6. Available at: https://link.springer.com/article/10.1007/s00767-011-0185-6

Wei, X., Yang, G., Hu, L. (2010). Drainage experiment numerical simulation and the model evaluation in the mining area based on FEFLOW. Ground Water (in Chinese), 5, 1-2+22. Available at: http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXSU201005000.htm