Use of Airborne, Surface, and Borehole Geophysical Techniques at Contaminated Sites
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Infiltration from the Pedon to Global Grid Scales: an Overview and Outlook for Land Surface Modeling
Published June 24, 2019 Reviews and Analyses Core Ideas Infiltration from the Pedon to Global • Land surface models (LSMs) show Grid Scales: An Overview and Outlook a large variety in describing and upscaling infiltration. for Land Surface Modeling • Soil structural effects on infiltration in LSMs are mostly neglected. Harry Vereecken, Lutz Weihermüller, Shmuel Assouline, • New soil databases may help to Jirka Šimůnek, Anne Verhoef, Michael Herbst, Nicole Archer, parameterize infiltration processes Binayak Mohanty, Carsten Montzka, Jan Vanderborght, in LSMs. Gianpaolo Balsamo, Michel Bechtold, Aaron Boone, Sarah Chadburn, Matthias Cuntz, Bertrand Decharme, Received 22 Oct. 2018. Agnès Ducharne, Michael Ek, Sebastien Garrigues, Accepted 16 Feb. 2019. Klaus Goergen, Joachim Ingwersen, Stefan Kollet, David M. Lawrence, Qian Li, Dani Or, Sean Swenson, Citation: Vereecken, H., L. Weihermüller, S. Philipp de Vrese, Robert Walko, Yihua Wu, Assouline, J. Šimůnek, A. Verhoef, M. Herbst, N. Archer, B. Mohanty, C. Montzka, J. Vander- and Yongkang Xue borght, G. Balsamo, M. Bechtold, A. Boone, S. Chadburn, M. Cuntz, B. Decharme, A. Infiltration in soils is a key process that partitions precipitation at the land sur- Ducharne, M. Ek, S. Garrigues, K. Goergen, J. face into surface runoff and water that enters the soil profile. We reviewed the Ingwersen, S. Kollet, D.M. Lawrence, Q. Li, D. basic principles of water infiltration in soils and we analyzed approaches com- Or, S. Swenson, P. de Vrese, R. Walko, Y. Wu, and Y. Xue. 2019. Infiltration from the pedon monly used in land surface models (LSMs) to quantify infiltration as well as its to global grid scales: An overview and out- numerical implementation and sensitivity to model parameters. -
Brief Communication: the Role of Geophysical Imaging in Local Landslide Early Warning Systems
https://doi.org/10.5194/nhess-2021-225 Preprint. Discussion started: 29 July 2021 c Author(s) 2021. CC BY 4.0 License. Brief communication: The role of geophysical imaging in local landslide early warning systems 1 2 1 3 1 Jim S. Whiteley , , Arnaud Watlet , J. Michael Kendall , Jonathan E. Chambers 1Shallow Geohazards and Earth Observation, British Geological Survey, Environmental Science Centre, Nicker Hill, 5 Nottingham, NG12 5GG, United Kingdom. 2School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol, BS8 1RJ, United Kingdom. 3University of Oxford, Department of Earth Sciences, South Parks Road, Oxford, OX1 3AN, United Kingdom Correspondence to: J.S. Whiteley ([email protected]) Abstract. We summarise the contribution of geophysical imaging to local landslide early warning systems (LoLEWS), 10 highlighting how LoLEWS design and monitoring components benefit from the enhanced spatial and temporal resolutions of time-lapse geophysical imaging. In addition, we discuss how with appropriate laboratory-based petrophysical transforms, these geophysical data can be crucial for future slope failure forecasting and modelling, linking other methods of remote sensing and intrusive monitoring across different scales. We conclude that in light of ever increasing spatiotemporal resolutions of data acquisition, geophysical monitoring should be a more widely considered technology in the toolbox of methods available to 15 stakeholders operating LoLEWS. 1 Introduction Landslide mitigation measures are broadly divided in to two types: engineering approaches to reduce frequency or intensity of failures; and vulnerability reduction measures that de-risk exposed elements (Pecoraro et al., 2019). Here we concentrate on the latter, through the use of landslide early warning systems (LEWS). -
Preprint Arxiv:1806.10939, 2018
Solid Earth Discuss., https://doi.org/10.5194/se-2019-4 Manuscript under review for journal Solid Earth Discussion started: 15 January 2019 c Author(s) 2019. CC BY 4.0 License. Bayesian geological and geophysical data fusion for the construction and uncertainty quantification of 3D geological models Hugo K. H. Olierook1, Richard Scalzo2, David Kohn3, Rohitash Chandra2,4, Ehsan Farahbakhsh2,4, Gregory Houseman3, Chris Clark1, Steven M. Reddy1, R. Dietmar Müller4 5 1School of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA 6845, Australia 2Centre for Translational Data Science, University of Sydney, NSW 2006 Sydney, Australia 3Sydney Informatics Hub, University of Sydney, NSW 2006 Sydney, Australia 4EarthByte Group, School of Geosciences, University of Sydney, NSW 2006 Sydney, Australia Correspondence to: Hugo K. H. Olierook ([email protected]) 10 Abstract. Traditional approaches to develop 3D geological models employ a mix of quantitative and qualitative scientific techniques, which do not fully provide quantification of uncertainty in the constructed models and fail to optimally weight geological field observations against constraints from geophysical data. Here, we demonstrate a Bayesian methodology to fuse geological field observations with aeromagnetic and gravity data to build robust 3D models in a 13.5 × 13.5 km region of the Gascoyne Province, Western Australia. Our approach is validated by comparing model results to independently-constrained 15 geological maps and cross-sections produced by the Geological Survey of Western Australia. By fusing geological field data with magnetics and gravity surveys, we show that at 89% of the modelled region has >95% certainty. The boundaries between geological units are characterized by narrow regions with <95% certainty, which are typically 400–1000 m wide at the Earth’s surface and 500–2000 m wide at depth. -
Guides to Understanding the Aeromagnetic Expression of Faults in Sedimentary Basins: Lessons Learned from the Central Rio Grande Rift, New Mexico
Guides to understanding the aeromagnetic expression of faults in sedimentary basins: Lessons learned from the central Rio Grande rift, New Mexico V.J.S. Grauch U.S. Geological Survey, MS 964, Federal Center, Denver, Colorado 80225-0046, USA Mark R. Hudson U.S. Geological Survey, MS 980, Federal Center, Denver, Colorado 80225-0046, USA ABSTRACT cho, northwest of Albuquerque, New Mexico (Fig. 2). Linear anomalies are interpreted as faults that offset basin-fi ll sediments based on their High-resolution aeromagnetic data acquired over several basins in consistent correspondence to isolated exposures of mapped faults, follow- the central Rio Grande rift, north-central New Mexico, prominently up investigations at individual sites, and geophysical modeling (Grauch, display low-amplitude (5–15 nT) linear anomalies associated with 2001; Grauch et al., 2001, 2006). faults that offset basin-fi ll sediments. The linear anomalies give an As in many sedimentary basins, mapping faults in the central Rio unparalleled view of concealed faults within the basins that has sig- Grande rift is diffi cult because of the extensive alluvial cover. As a conse- nifi cant implications for future basin studies. These implications pro- quence, geologists have used the linear aeromagnetic anomalies to delin- vide the impetus for understanding the aeromagnetic expression of eate partially concealed faults and denote possible locations of totally faults in greater detail. Lessons learned from the central Rio Grande buried faults on geologic maps (e.g., Connell, 2006) and in fault compila- rift help to understand the utility of aeromagnetic data for examin- tions (Machette et al., 1998; Personius et al., 1999). -
Geophysical Imaging of Permafrost in the SW Svalbard – the Result of Two High Arctic Expeditions to Spitsbergen
EGU2020-8136, updated on 25 Sep 2021 https://doi.org/10.5194/egusphere-egu2020-8136 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Geophysical imaging of permafrost in the SW Svalbard – the result of two high arctic expeditions to Spitsbergen Mariusz Majdanski1, Artur Marciniak1, Bartosz Owoc1, Wojciech Dobiński2, Tomasz Wawrzyniak1, Marzena Osuch1, Adam Nawrot1, and Michał Glazer2 1Institute of Geophysics, Polish Academy of Sciences, Warsaw, Poland ([email protected]) 2Department of Earth Sciences, University of Silesia, Sosnowiec, Poland The Arctic regions are the place of the fastest observed climate change. One of the indicators of such evolution are changes occurring in the glaciers and the subsurface in the permafrost. The active layer of the permafrost as the shallowest one is well measured by multiple geophysical techniques and in-situ measurements. Two high arctic expeditions have been organized to use seismic methods to recognize the shape of the permafrost in two seasons: with the unfrozen ground (October 2017) and frozen ground (April 2018). Two seismic profiles have been designed to visualize the shape of permafrost between the sea coast and the slope of the mountain, and at the front of a retreating glacier. For measurements, a stand-alone seismic stations has been used with accelerated weight drop with in- house modifications and timing system. Seismic profiles were acquired in a time-lapse manner and were supported with GPR and ERT measurements, and continuous temperature monitoring in shallow boreholes. Joint interpretation of seismic and auxiliary data using Multichannel analysis of surface waves, First arrival travel-time tomography and Reflection imaging show clear seasonal changes affecting the active layer where P-wave velocities are changing from 3500 to 5200 m/s. -
Geophysics (3 Credits) Spring 2018
GEO 3010 – Geophysics (3 credits) Spring 2018 Lecture: FASB 250, 10:45-11:35 am, M & W Lab: FASB 250, 2:00-5:00 pm, M or W Instructor: Fan-Chi Lin (Assistant Professor, Dept. of Geology & Geophysics) Office: FASB 271 Phone: 801-581-4373 Email: [email protected] Office Hours: M, W 11:45 am - 1:00 pm. Please feel free to email me if you would like to make an appointment to meet at a different time. Teaching Assistants: Elizabeth Berg ([email protected]) FASB 288 Yadong Wang ([email protected]) FASB 288 Office Hours: T, H 1:00-3:00 pm Website: http://noise.earth.utah.edu/GEO3010/ Course Description: Prerequisite: MATH 1220 (Calculus II). Co-requisite: GEO 3080 (Earth Materials I). Recommended Prerequisite: PHYS 2220 (Phycs For Scien. & Eng. II). Fulfills Quantitative Intensive BS. Applications of physical principles to solid-earth dynamics and solid-earth structure, at both the scale of global tectonics and the smaller scale of subsurface exploration. Acquisition, modeling, and interpretation of seismic, gravity, magnetic, and electrical data in the context of exploration, geological engineering, and environmental problems. Two lectures, one lab weekly. 1. Policies Grades: Final grades are based on following weights: • Homework (25 %) • Labs (25 %) • Exam 1-3 (10% each) • Final (20 %) Homework: There will be approximately 6 homework sets. Homework must be turned in by 5 pm of the day they are due. 10 % will be marked off for each day they are late. Homework will not be accepted 3 days after the due day. Geophysics – GEO 3010 1 Labs: Do not miss labs! In general you will not have a chance to make up missed labs. -
Geophysics 210 September 2008
Geophysics 210 September 2008 Geophysics 210 - Physics of the Earth A1: What is geophysics Geophysics: Application of physics to understand the structure and working of the Earth. Geophysics can be divided into exploration geophysics and geodynamics. Exploration geophysics is the process of imaging what is inside the Earth. Direct sampling in the Earth with drilling can only reach depths around 10 km so indirect methods are needed. Often used to describe commercial exploration, but includes investigations to depths of the mantle and core. All geophysical methods can be divided into active and passive techniques. In an active technique, it is necessary to generate a signal (e.g. in seismic studies sound waves are generated with an explosion or an earthquake). In a passive technique a naturally occurring signal is detected (e.g. the pull of gravity of a buried object). Geodynamics is the study of how the Earth works, and considers questions such as: -what drives plate motion? -what triggers earthquakes? -how is the Earth’s magnetic field generated? -how do continent-continent collisions build mountains? This field depends heavily on information derived from geophysical imaging. Advances in computer power now allow simulations of these processes in ever increasing detail and realism. A2 : Basic structure of the Earth • Radially symmetric to first order. • Crust – mainly silicate minerals, enriched in lighter elements (Na, Al) • Mantle – silicate minerals with more heavy elements (Fe and Mg) magnesium. Divided into upper and lower mantle (dashed line) • Outer core - liquid iron that convects rapidly. • Inner core – Lump of solid iron roughly the size of the moon • Crust and mantle are defined in terms of their distinct chemical compositions. -
Time-Lapse Seismic and Electrical Monitoring of the Vadose Zone During a Controlled Infiltration Experiment at the Ploemeur Hydrological Observatory, France
water Article Time-Lapse Seismic and Electrical Monitoring of the Vadose Zone during a Controlled Infiltration Experiment at the Ploemeur Hydrological Observatory, France Lara A. Blazevic 1,2,*, Ludovic Bodet 2, Sylvain Pasquet 3 , Niklas Linde 4, Damien Jougnot 2 and Laurent Longuevergne 1 1 CNRS, Géosciences Rennes—UMR 6118, Université Rennes, F-35000 Rennes, France; [email protected] 2 CNRS, EPHE, METIS, Sorbonne Université, F-75005 Paris, France; [email protected] (L.B.); [email protected] (D.J.) 3 Institut de physique du globe de Paris, CNRS, Université de Paris, F-75005 Paris, France; [email protected] 4 Institute of Earth Sciences, University of Lausanne, CH-1015 Lausanne, Switzerland; [email protected] * Correspondence: [email protected] Received: 31 March 2020; Accepted: 21 April 2020; Published: 25 April 2020 Abstract: The vadose zone is the main host of surface and subsurface water exchange and has important implications for ecosystems functioning, climate sciences, geotechnical engineering, and water availability issues. Geophysics provides a means for investigating the subsurface in a non-invasive way and at larger spatial scales than conventional hydrological sensors. Time-lapse hydrogeophysical applications are especially useful for monitoring flow and water content dynamics. Largely dominated by electrical and electromagnetic methods, such applications increasingly rely on seismic methods as a complementary approach to describe the structure and behavior of the vadose zone. To further explore the applicability of active seismics to retrieve quantitative information about dynamic processes in near-surface time-lapse settings, we designed a controlled water infiltration experiment at the Ploemeur Hydrological Observatory (France) during which successive periods of infiltration were followed by surface-based seismic and electrical resistivity acquisitions. -
Ten Years of Marine CSEM for Hydrocarbon Exploration
GEOPHYSICS, VOL.75, NO. 5 ͑SEPTEMBER-OCTOBER 2010͒; P.75A67–75A81, 15 FIGS. 10.1190/1.3483451 Ten years of marine CSEM for hydrocarbon exploration Steven Constable1 years of the first survey three contracting companies had been ABSTRACT formed for the express purpose of providing commercial marine CSEM services to the exploration industry. Now, almost 10 years af- Marine controlled-source electromagnetic ͑CSEM͒ sur- ter the Girassol survey, marine CSEM is a broadly used, if not main- veying has been in commercial use for predrill reservoir ap- stream, geophysical technology, with over 500 surveys reportedly praisal and hydrocarbon exploration for 10 years.Although a having been carried out and several custom-built survey vessels in recent decrease has occurred in the number of surveys and operation. The 75th anniversary of GEOPHYSICS and the 10th anni- publications associated with this technique, the method has versary of commercial marine CSEM seem to constitute an appro- become firmly established as an important geophysical tool priate occasion to review the marine CSEM method: where we have in the offshore environment. This is a consequence of two im- been, where we are today, and where we might be going. portant aspects associated with the physics of the method: The aim of this paper is to provide a technical review, which is ac- First, it is sensitive to high electrical resistivity, which, al- cessible to the nonexpert, of the marine CSEM method. However, to though not an unambiguous indicator of hydrocarbons, is an illustrate some of the important issues, original calculations have important property of economically viable reservoirs. -
SOP14 Geophysical Survey
SSFL Use Only SSFL SOP 14 Geophysical Survey Revision: 0 Date: April 2012 Prepared: C. Werden Technical Review: J. Plevniak Approved and QA Review: J. Oxford Issued: 4/6/2012 Signature/Date 1.0 Objective The purpose of this technical standard operating procedure (SOP) is to introduce the procedures for non-invasive geophysical investigations in areas suspected of being used for disposal of debris or where landfill operations may have been conducted. Specifics of the geophysical surveys will be discussed in the Geophysical Survey Field Sampling Plan Addendum. Geophysical methods that will be used to accurately locate and record buried geophysical anomalies are: . Total Field Magnetometry (TFM) . Frequency Domain Electromagnetic Method (FDEM) . Ground Penetrating Radar (GPR) TFM and FDEM will be applied to all areas of interest while GPR will be applied only to areas of interest that require further and/or higher resolution of geophysical anomaly. The geophysical investigation (survey) will be conducted by geophysical subcontractor personnel trained, experienced, and qualified in shallow subsurface geophysics necessary to successfully perform any of the above geophysical methods. CDM Smith will provide oversight of the geophysical contractor. 2.0 Background 2.1 Discussion This SOP is based on geophysical methods employed by US Environmental Protection Agency’s (EPA) subcontractor Hydrogeologic Inc. (HGL) while conducted geophysical surveys of portions of Area IV during 2010 and 2011. The Data Gap Investigation conducted as part of Phase 3 identified additional locations of suspected buried materials not surveyed by HGL. To be consistent with the recently collected subsurface information, HGL procedures are being adopted. The areas of interest and survey limits will be determined prior to field mobilization. -
Modeling for Inversion in Exploration Geophysics A
MODELING FOR INVERSION IN EXPLORATION GEOPHYSICS A Dissertation Presented to The Academic Faculty By Mathias Louboutin In Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the School of CSE in the College of Computing Georgia Institute of Technology February 2020 Copyright c Mathias Louboutin 2020 MODELING FOR INVERSION IN EXPLORATION GEOPHYSICS Approved by: Dr. Felix J. Herrmann, Advisor School Computational Science and Engineering Dr. Tobin Isaac Georgia Institute of Technology School of Computer Science Georgia Institute of Technology Dr. Umit Catalyurek School Computational Science and Dr. Zhigang Peng Engineering School of Earth and Atmospheric Georgia Institute of Technology Sciences Georgia Institute of Technology Dr. Edmond Chow School Computational Science and Date Approved: March 1, 2020 Engineering Georgia Institute of Technology ACKNOWLEDGEMENTS Before anything else, I would like to thank my supervisor Dr Felix J. Herrmann for giv- ing me the opportunity to work with him. Thanks to his leadership I had the opportunity to work and scientifically challenging problems in a collaborative and motivating atmosphere. I would also like to thank Professor Gerard Gorman at Imperial college. And large part of my research was kick-started by a visit at Imperial College and Dr. Gorman’s support and guidance made me achieve my research objective. I would like to thank Professor Umit Catalyurek, Professor Edmond Chow, Professor Tobin Isaac and Professor Zhigang Peng for agreeing to be on my Ph.D. committee at Georgia Tech, for reviewing my thesis, for making time for my proposal and defense and for your valuable input on my work. I would also like to thank my former Ph.D. -
Results of the Application of Seismic- Reflection And
RESULTS OF THE APPLICATION OF SEISMIC- REFLECTION AND ELECTROMAGNETIC TECHNIQUES FOR NEAR-SURFACE HYDROGEOLOGIC AND ENVIRONMENTAL INVESTIGATIONS AT FORT BRAGG, NORTH CAROLINA ByM.T. Meyer and Jason M. Fine U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 97-4042 Prepared for the Department of the Army Fort Bragg, North Carolina Raleigh, North Carolina 1997 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey. For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 3916 Sunset Ridge Road Box 25286 Raleigh, NC 27607 Denver Federal Center Denver, CO 80225-0286 CONTENTS Page Abstract.................................................................................. 1 Introduction.............................................................................. 2 Background ....................................................................... 3 Purpose and scope ................................................................. 3 Physiographic and geologic settings .................................................. 4 Acknowledgments .............................................................. 6 Surface-geophysical methods ............................................................... 7 Shallow seismic reflection