Mark Person running Transient Electro Magnetic Survey on the Island of Comino, Malta,
H510 Quantitative Methods in Hydrology: This class provides students with an introduction to analytical and numerical methods
used in the hydrologic sciences. We will begin by considering relatively simple descriptions
of hydrologic systems using ordinary differential equations (ODEs) where the independent
variable is either space (x) or time (t). Building on what you learned in calculus,
we will find both analytical and numerical solutions to these ODEs. Next we will consider
more complicated hydrologic systems involving two independent variables (either x
& z or x & t). These are described using partial differential equations (PDEs). We
will find both analytical and numerical solutions to the PDEs.
HYD 547 Hydrological Modeling: Introduction to the finite difference (FD), finite element (FE), and Control Volume
finite element methods applied to groundwater flow, heat and solute transport equations
in two- (2D) and three- (3D) spatial dimensions. Analysis and synthesis of hydrologic
data using mathematical modeling. Topics covered include model conceptualization and
parameterization, model verification, model validation, and model prediction. Students
will be exposed to the following modeling packages: MATLAB and MODFLOW. Students will be expected to develop MATLAB programs to solve a variety of simple 2D finite element and finite difference approximations
of flow and transport problems.
HYD 516: Geofluids: The Role of Groundwater in Geologic Processes: This class will explore different fluid flow impelling mechanisms within the earth’s
crust to depths of 10 km. Topics covered would include the role of groundwater in
petroleum generation/migration, overpressure/underpressure formation in sedimentary
basins, hydrothermal ore deposit formation, contact metamorphism, geothermal systems,
seismicity, slope failure, sediment transport, and glaciation.
Research Interests: Paleohydrology, low-temperature geothermal systems, induced seismicity, hydrogeophysics,
and numerical methods.
My research interests are primarily focused on studying how groundwater flow systems
evolve over geologic time scales and how subsurface flow systems affect geologic processes.
One focus of my research has been centered on assessing how Pleistocene glaciations
have influenced regional groundwater flow systems within sedimentary basins (Person
et al. 2007; Bense and Person, 2008) and on the continental shelf (Person et al. 2003;
Cohen et al. 2009; Defoor et al. 2011; Post et al. 2013). While this topic may sound
esoteric, it is relevant coastal cities in arid regions of the world as well as to
high-level nuclear waste repository siting efforts in countries such as Sweden, Canada,
and Switzerland. Another focus of my work has been on assessing the role of groundwater
flow in petroleum generation (Person and Garven, 1992; Person et al. 1995), petroleum
migration (Person et al. 2012), and triggered seismicity (Zhang et al. 2013; 2017).
I am also interested in how permeable fault systems affect groundwater flow and hot
spring formation within the extensional tectonic settings (Bense et al. 2008; Person
et al. 2012; Howald et al. 2012; Pepin et al. 2015). In 2014, my lab acquired a magnetotelluric,
audio-magnetotelluric (AMT), transient electromagnetic (TEM) system from Zonge International.
Zonge International (http://zonge.com/). Along with Dr. Shari Kelley of the NM Bureau of Geology & Mineral Resources and
assistant professor Jesus Gomez-Velez, we are using these systems to study deep groundwater
flow systems within fractured crystalline basement rocks along the Rio Grande Rift.
I have been actively involved in developing new hydrologic models that reconstruct
groundwater flow system during the geologic past. Early in my career, my graduate
students and I developed RIFT2D (Wieck et al. 1995; Mailloux et al. 1999), a Fortran based groundwater flow code which
simulates basin evolution (i.e. sedimentation, subsidence, erosion) along with heat
and solute transport within evolving continental rift basins. More recently, Denis
Cohen, Peng Wang and I developed PGEOFE. This three-dimensional groundwater flow model is parallel and represents variable-density
groundwater flow, heat and solute transport over geologic time scales. We used this
model to simulate the emplacement of freshwater in continental shelf environments
in New England during periods of glaciations (Cohen et al. 2009). Currently I am developing
a control volume finite element model with professor Vaughan Voller at the University
of Minnesota and Yipeng Zhang (doctoral student). We are using this hydromechanical
code to study the effects of ice sheet loading on groundwater flow and rock failure/permeability
increases during the Pleistocene glaciations.
(A) Base map showing location of cross sections used to construct a three-dimensional
PGEOFE groundwater flow model of New England Continental Shelf. (B) Hydrostratigraphic cross
sections showing clay (blue), sand (green) and silt (red) deposits. (C) Computed present-day
salinity patterns on New England continental shelf. From Cohen et al. (2009).
Three-dimensional, high-performance hydrogeologic model of the New England continental
shelf, USA used by Cohen et al. (2009) to estimate the volume of freshwater sequestered
within permeable sand horizons during Pleistocene glaciations and sea level fluctuations
(1300 cubic km). The bottom figure in the left panel shows the PGEOFE numerical grid (about 1.3 million nodes), hydrostratigraphic units (blue, green, red
patterns), bathymetry (top figure), and the Laurentide ice sheet thickness (middle
figure) 21,000 years ago. The center panel shows the hydrostratigraphic unit configuration
along 7 cross-sectional transects through the model domain. The right panel shows
the present-day computed salinity distribution. The models were calibrated to off-shore
salinity profiles from a number of wells (cylinders).
Birdsall-Dreiss Distinguished Lecturer, Geological Society of America, 1997
New Mexico Tech Distinguished Research Award, 2016
Editor, Geofluids, Blackwell-Wiley, 2011-2016
National Science Foundation, $2.1M, 2019-2022, Collaborative Research: Exploring the linkages between Sea-Level Change, Sediment
Transport and Geomorphology on Coastal Freshwater Water Sequestration Natural climatic fluctuations have induced sea-level oscillations
of more than hundred meters during the past million years. As sea level rose and fell,
the shoreline moved landward and seaward shifting the boundary between fresh water
onshore and salt water offshore. As a result, saline groundwater is found beneath
coastal zones onshore and freshwater is found offshore. While saltwater intrusion
in onshore freshwater aquifers has been extensively studied, we know little about
the mechanisms responsible for the emplacement of fresh to brackish water in marine
environments. We estimate that there is over 100,000 km3 of freshwater stored in offshore sandy sediments around the world. To put this number
in perspective, the total estimated annual groundwater withdrawal from on shore aquifers
within the United States in 2015 was 117 km3. Offshore freshwater represents a vast untapped, albeit non-renewable water resource,
for coastal megacities. This project will assess how the sequestration of onshore
saltwater and offshore freshwater in continental shelf environments is influenced
by interactions between sea level, the changing landscape, deposition of sediments,
and surface and subsurface water flow over time scales of a million years or more.
In order to assess these interactions, we will build a mathematical model to understand
the dynamic linkages between the above-mentioned components of the Earth system. We
will develop a new model using the earth science community code, Landlab, and apply the code at two field sites with vastly different local sea-level, climate,
tectonic and sediment transport regimes: New Jersey and Bangladesh. Calculated sediment
type and salinity patterns from these models will be compared to new and existing
images from seismic data and electromagnetic (EM) data, as well as available well
samples measuring salinity and age of the water. EM data is very sensitive to how
salty or fresh water is. We will conduct an EM survey in Bangladesh to determine the
distribution of deep onshore saltwater and freshwater in this active deltaic environment.
Along with recently collected EM images from offshore New Jersey, these data will
be used to inform and constrain our numerical modeling. We will also develop three-dimensional
models of groundwater production for New Jersey and Bangladesh to assess whether or
not offshore freshwater can be efficiently produced using horizontal wells over time
scales of 30 years or more. Our study has important societal impacts for coastal
cities in Bangladesh such as Chittagong and Barisal, which are growing rapidly and
are running out of drinking water of acceptable quality.
European Union Science Agency, €1.7M, 2017-2022, MACRAN: Topographically-driven meteoric groundwater – an important
geomorphic agent. Dr. Aaron Micallef (PI), University of Malta, Mark Person (co-PI), NM Tech. This
project focuses on understanding the role of groundwater as a geomorphic agent in
continental shelf environments and the emplacement of submarine freshwater resources
during Pleistocene sea-level low stands (www.marcan.eu). The study focuses on two study site offshore New Zealand (south Island) and near
Malta. One specific goal of this project is to develop three-dimensional characterizations
of the volume of sequestered freshwater on Malta’s continental shelf.
Keck Foundation, $1M, 2017-2020, Evolution of Crustal Paleofluid Systems, $1M, Peter Reiner, University
of Arizona (PI), Mark Person (co-PI), NM Tech. This project focuses on the role of
Geofluids (oil, methane, supercritical CO2, and saline brines) as an agent in the
formation of world class uranium and copper deposits within the Paradox Basin, Utah.
Defense Threat Reduction Agency (DTRA), $630K, 2017-2020, Integration of Noble Gas and Seismic Measurements for Small Yield
Event Discrimination and Yield Estimation: A Multidisciplinary Experimental Study.
Anastasia Stroujkova (PI), Weston Geophysical. Mark Person and Jesus Gomez-Velez (co-PIs),
New Mexico Tech. This multidisciplinary project focuses on characterizing gas migration
(SF6) released above and below the water table in fractured granitic rocks as well
as seismic wave propagation following the detonation of conventional explosives emplaced
beneath the land surface.
Current Graduate Students
Natalie Camile, BS Geology, University of Wyoming
Elizabeth Evenocheck, BS Geology, Winona State University
Dolan Lucero, BS Geology, University of Utah
Navis Sazeed. BS Disaster Science, University of Dhaka
Melinda Horne, 2019, Montana Department of the Environment,
Sofia Avendano, 2019, Los Alamos National Laboratory
Matt Folsom, MSc. 2017, ORMAT, Reno NV
John Ortiz, MSc. 2017, Johns Hopkins University
Dr. Amy Jordan, Ph.D. 2016, Neptune LLC, Los Alamos NM
David Bulter, MSc. 2014, CH2M-Hill, Seattle WA
Yipeng Zhang, Ph.D., Postdoc, University of Malta
Jeff Pepin, Ph.D., US Geological Survey, Albuquerque, NM
Bense V. F., M. Person (2006), Faults as conduit-barrier systems to fluid flow in siliciclastic sedimentary
aquifers, Water Resources Research, 42, W05421, doi:10.1029/2005WR004480
Bense V. F., M. A. Person, K. Chaudhary, Y. You, N. Cremer, S. Simon (2008), Thermal anomalies indicate preferential
flow along faults in unconsolidated sedimentary aquifers, Geophys. Res. Lett., 35,
Bense V. F., M. A. Person (2008), Transient hydrodynamics within intercratonic sedimentary basins during glacial
cycles, J. Geophys. Res., 113, F04005, doi:10.1029/2007JF000969
Cohen, D., Person M. , Wang, P. Gable, C. Hutchinson, D., Marksamer, A. Dugan, B. Kooi, H. Groen, K.,
Lizarralde, D. and R. L. Evans, Origin and Extent of Fresh Paleowaters Beneath the
Atlantic Continental Shelf, 2009, Groundwater, Volume 48 Issue 1, p. 143 – 158
DeFoor, W. Person, M., Larsen, H.C., Lizarralde, D. Cohen, D. and B. Dugan, 2011, Ice sheet–derived submarine
groundwater discharge on Greenland’s continental shelf, Water Resources Research,
Howald T, Person M, Campbell A, Lueth V, Hofstra A, Sweetkind D, Gable CW, Banerjee A, Luijendijk E,
Crossey L, Karlstrom K, Kelley S, and Phillips F, 2014. Evidence for Long-Time Scale
( > 103 years) Changes in Hydrothermal Activity Induced by Seismic Events, Geofluids, doi:
Post, V. Groen, J., Kooi, H. Person, M., Ge, S. 2013, Review: Offshore fresh groundwater reserves – A global phenomenon,
Nature, v. 504, p. 71-84, doi:10.1038/nature12858
Jordan, A, Stauffer, P, Zyvoloski, G, Person, M. MacCarthy J, and Anderson, D, 2014, Uncertainty in Prediction of Radionuclide Gas
Migration from Underground Nuclear Explosions, Vadose Zone J. doi:10.2136/vzj2014.06.0070
Person, M. and G. Garven, 1992, Hydrologic constraints on petroleum generation within continental
rift basins: Theory and application to the Rhine Graben, American Association of Petroleum
Geologists Bulletin, v. 76, p. 468–488
Person, M., Toupin, D., and Eadington, P. J., 1995, One–dimensional models of groundwater flow,
sediment thermal history, and petroleum generation within continental rift basins, Basin Research, v. 7, p. 81-96.
Person, M., Dugan, B., Swenson, J.B., Urbano, L., Sttot, C., Taylor, J., Willett, M., 2003,
Pleistocene hydrogeology of the Atlantic continental shelf, New England, GSA Bulletin, v. 115. p. 1324-1343.
Person M., J. McIntosh, V. Bense, V. H. Remenda, 2007, Pleistocene hydrology of North America:
The role of ice sheets in reorganizing groundwater flow systems, Rev. Geophys., 45,
Person M. , Hofstra, A., Sweetkind, D, Stone, W., Cohen, D., Gable, C, Banerjee, A. 2012, Analytical
and numerical models of hydrothermal fluid flow at fault intersections, Geofluids,
v. 12, 312–326
Person, M. Butler, D., Gable, C. W., Villamil, T., Waverek, D., and D. Schelling, 2012, Hydrodynamic stagnation zones: A new play concept forthe Llanos Basin, Colombia, Association
of Petroleum Geologists Bulletin, v. 96 no. 1 p. 23-41.
Pepin J, Person M, Phillips F, Kelley S, Timmons S, Witcher J, and Gable C, 2014, Deep Fluid Circulation
within Crystalline Basement Rocks and the Role of Hydrologic Windows in the Formation
of the Truth or Consequences, New Mexico Low-Temperature Geothermal System, Geofluids,
Zhang, Y., Person, M., Rupp, J., Ellet, K., Celia, M.A., Gable, C.W., Bowen, B., Evans, J., Bandilla,
K., Mozley, P.S., Dewers, T., and Elliot, T., 2013, Hydrogeologic controls on induced
seismicity in crystalline basement rocks due to fluid injection into basal reservoirs: Groundwater, v. 51, Issue 4, p. 525–538.
Zhang, Y., S. Edel, J. Pepin, M. Person, et al., “Exploring the potential linkages between oil‐field brine reinjection, crystalline
basement permeability, and triggered seismicity for the Dagger Draw Oil field, doi: