Geophysical Survey Techniques to Determine Lengths of Piles and Drilled Shafts

Author(s):  
Edward J. Mercado ◽  
Michael W. O'Neill
2017 ◽  
Vol 97 ◽  
pp. 27-47
Author(s):  
Kirsty Millican ◽  
Helen Goodchild ◽  
Dorothy Graves McEwan

This paper presents the results of a survey project investigating a complex of prehistoric archaeological sites at Lochbrow, in Dumfries and Galloway, Scotland. An Early Neolithic timber cursus, Late Neolithic or Early Bronze Age timber circles and Bronze Age round barrows were first recorded as cropmarks on aerial photographs in the 1980s and 1990s. The Lochbrow Landscape Project set out to investigate and understand this lesser-known complex of prehistoric sites and their layout in the landscape using non-destructive survey techniques, including geophysical survey, experiential survey and re-assessment of aerial photographs. A pilot survey was undertaken in 2010 followed by a series of short field seasons from 2011 to 2015. Interpretation of the results from geophysical survey has proved challenging because of strong geological and geomorphological signals, but has been successful in detecting both the features known from aerial photographs and additional archaeological features. The simple step of marking out the known archaeology on the ground has provided additional insights into the landscape context of the known monuments and elements of their morphology. This indicates that the monuments were closely tied to their landscape context and that the monument boundaries were used to influence the experience of being within the monuments. Overall, the research has been successful in enriching our understanding of the complex of prehistoric sites known at Lochbrow.


2020 ◽  
Author(s):  
Ben Dashwood ◽  
Cornelia Inauen ◽  
Arnaud Watlet ◽  
Itzel Isunza Manrique ◽  
David Caterina ◽  
...  

<p><span>The future mining potential of a landfill site requires the assessment of the likely volume and distribution of recoverable materials of value, within an overall waste body. Whilst more recently constructed landfill sites may have some record of the type and volume of waste deposited, as well as information concerning the extent of an overall site, there is often scant information available for older landfills. For such sites, the potential for the recovery of waste materials will require some form of rapid characterisation (valorisation) of the waste, such that the cost-effectiveness of any mining operation may be estimated.</span></p><p><span>Geophysical survey techniques offer the potential to rapidly delineate variations in material properties and may be deployed at a range of scales to suit the dimensions of a site or expected level of heterogeneity within the waste. The majority of geophysical techniques are also non-invasive, which is particularly important where potentially hazardous waste is expected, or where the integrity of environmental protection measures such as geotextile membranes must be maintained. </span></p><p><span>This case study presents the application of number of geophysical survey techniques to characterise the waste within a filled portion of an active landfill in Normandy, France (Les Champs Jouault) and is a pilot site for the RAWFILL project. The site has been operational since April 2009 and was chosen in part due to the large volume of information concerning the construction and nature of the waste materials deposited. This permitted a reasonably well-constrained interpretation of the geophysical data collected. The site poses a number of interesting issues relating to the fact that the site generates and harvest biogas/methane from the waste materials utilising an injected/recirculated leachate system, with individual waste cells fully sealed with an impermeable geomembrane (liner), which also sits above the waste and is then covered with natural soils. The presence of the liner above the waste prohibited the use of Electrical Resistivity Tomography (ERT) for the geophysical characterisation. </span></p><p><span>The case study presented used multiple phases of geophysical survey to characterise the solid waste, as well as to target intrusive sampling undertaken at the site. A number of geophysical techniques were applied, including Ground Penetrating Radar (GPR), Electro-Magnetic (EM) and Magnetic techniques, as well as seismic techniques (Multi-channel Analysis of Surface Waves (MASW) and Horizontal to Vertical Signal Ratio (HVSR)). The initial survey provided valuable information concerning the thickness of cover above the geomembrane across the survey area, the extent of individual cells as well as variations in waste condition/composition within individual cells and the overall thickness of waste materials/depth to subgrade/bedrock. </span></p><p><span>The measured geophysical properties have been used to model both the lateral and vertical extents of the landfill as well as to map the distribution of material properties (potential resource). Preliminary findings were used to target a tranche of intrusive sampling (and further geophysical investigation) designed to ground-truth the geophysical data, with the knowledge gained from this exercise used to valorise the potentially recoverable waste materials present in the form of a Resource Distribution Model (RDM).</span></p><p> </p>


Geophysics ◽  
2012 ◽  
Vol 77 (3) ◽  
pp. B135-B146 ◽  
Author(s):  
Çağlayan Balkaya ◽  
Gökhan Göktürkler ◽  
Zülfikar Erhan ◽  
Yunus Levent Ekinci

Geophysical survey techniques have been successfully applied to near-surface cave detection in karstic terrains. We used magnetic and electrical resistivity surveys to delineate the karstic structure of the Ayvacık Sinkhole, which may be considered to be a vertical cave. The magnetic-total-field-anomaly map helped reveal the metamorphic and sedimentary units in the study area. The total-horizontal-gradient map, which was based on a calculated pseudogravity anomaly, successfully identified the contact between the limestone unit and the cave system. Using these results, we positioned and carried out a vertical electrical sounding (VES) survey with a Schlumberger array along a line that consisted of 11 stations. The VES data were then processed using a 1D global optimization technique, which used a genetic algorithm and a 2D linearized least-squares algorithm. The results were generally in good agreement with each other, and together they pointed out three geologic layers: (1) an overburden layer ([Formula: see text]), (2) an approximately 25-m-thick alluvial fill (100–316 Ωm), and (3) a limestone unit (316–3162 Ωm); and also suggested the existence of a high-resistive anomaly ([Formula: see text]), possibly a karstic cave, located at the depth of approximately 40 m. Also, the results suggested that the buried limestone unit had an undulating karstic topography including a probable pinnacle structure. A synthetic modeling study was carried out, and it validated the reliability of the results. Finally, our findings indicated that the geophysical survey techniques used here were successful in detecting a cave located deep enough to make human exploration difficult.


1979 ◽  
Vol 24 (12) ◽  
pp. 1053-1053
Author(s):  
JOHN W. COTTON

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