Abstract
Taking the 1950 Geological Society of America Berkey Volume on The Application of Geology to Engineering Practice as the baseline for the world-wide state of the art at that time, this paper examines some of the significant advances in engineering geological practice that have taken place over the intervening period in the UK. The central role of advances in site investigation for development and construction is emphasized, as this can be reasonably described as the core activity for engineering geologists. Here the changes in desk studies, remote sensing, field mapping and various facets of ground investigations are examined. However, it is also necessary to highlight how global developments in communications and computing power have had an enormous impact on engineering geological practice, notably through on-site links between field teams and head office, and the creation of data management systems that allow complex ground conditions to be analysed and modelled. There have also been important improvements in on-site health and safety, the creation of professional qualifications and the adoption of international and national standards for all facets of ground engineering. Finally, some of the challenges engineering geology and its practitioners face in the future are explored, notably the implications of Industry 4.0, the changes that climate change will bring to society, training the next generation and ensuring that engineering geology remains a vibrant and globally recognized profession.
Those who cannot remember the past are condemned to repeat it (Santayana 1905–06).
The 2018 conference of the Engineering Group of the Geological Society of London (EGGS), held at Cambridge University in April, was on the subject of ‘keeping lessons alive’. This present paper was the invited keynote presentation that explored some of the advances that have occurred in the discipline. The history of engineering geology has been discussed in a number of publications including those by Kiersch (1991a), VanDine et al. (2006), Culshaw et al. (2008), Turner (2008) and Griffiths (2014). Although the first book on engineering geology was produced in London in the 19th century (Penning 1880), it was not until after the Second World War that the subject really emerged as a coherent discipline in the UK. Prior to that most of the developments in the subject took place elsewhere in Europe, notably including mapping in the USSR (Popov et al. 1950), or in the USA. The situation in the USA immediately after the Second World War was summarized in a remarkable book entitled Application of Geology to Engineering Practice (Paige 1950) produced in honour of one of the true pioneers in engineering geology, Charles P. Berkey (Fig. 1), and fittingly the book is known as the Berkey Volume. It is this volume that provides the baseline against which the present paper examines some of the important advances in engineering geology that have taken place in the UK over the past nearly 70 years. Although engineering geology has a demonstrably key role in mining engineering (Eggers 2016) and land contamination studies (Nathanail 2013), in line with the Engineering Group's general theme of the conference this paper focuses on those developments related to civil engineering. Also, because the advances have been extensive and complex this paper concentrates on only a few key areas: site investigation; communication and data management; health and safety; and professionalism. However, before these areas are explored it is necessary to review some of the pertinent aspects of the Berkey Volume.
Charles P. Berkey: Engineering Geologist (1867–1955) (image from the biography by Savage & Rhodes 1950).
The Berkey Volume
The Berkey Volume (Paige 1950) published by the Geological Society of America represented a superb compilation of the state of the art of engineering geology in the USA. At that time the USA was arguably the most advanced country in the world in using geologists to provide input to engineering projects. The contents of the volume are listed in Table 1 and include papers on the engineering geologist in engineering organizations, in route alignment studies, dams and tunnel construction, and coastal engineering. There is a paper by the ‘father of soil mechanics’ Karl Terzaghi on landslides (Terzaghi 1950). Terzaghi was always of the opinion that engineering geology and geotechnics were inextricably linked, a view he expounded in the first edition of Géotechnique (Terzaghi 1948).
Contents of the Berkey Volume (Paige 1950)
Some quotes from the Berkey Volume are presented below, as they provide an insight into the role of the engineering geologist and the state of the art in 1950.Engineering geology is not a branch of the science of geology: it is the practical application of all the branches of the science to the practical problems of engineering. Physiography [geomorphology], historical geology, stratigraphy, structural geology, petrography, economic geology, groundwater hydrology [hydrogeology] and even palaeontology – all the divisions of the science have important applications in civil engineering (Burwell & Roberts 1950, p. 2).
This shows that to be a good engineering geologist first and foremost a practitioner must be a good all-round geologist. The main point is that engineering geology is not a simplified version of geology. Engineering geologists require expertise in all aspects of the subject along with an ability to compile, interpret and integrate information from a wealth of allied Earth science disciplines and apply that understanding to practical problems in planning, civil engineering, resource assessment and mining.The geologist must be willing to advance information wherever it is requested and volunteer applicable information in anticipation of the engineer's needs (Burwell & Roberts 1950, p. 4).
This quote goes on to indicate that incomplete geological information on time is worth far more than complete information after decisions have been made. This shows that engineering geology even in 1950 was not regarded as an academic exercise, but as a ‘real-world discipline’ that needed to take account of the practical realities of construction schedules and budgets.It is an important function and responsibility of the geologist in the civil engineering organisation to see to it that contract plans and specifications adequately provide for all subsurface conditions that may be reasonably anticipated from the geological investigations (Burwell & Roberts 1950, p. 7).
The integration of the engineering geologist into the team drawing up contracts and specifications was regarded as normal practice. Thus, again engineering geology is seen as an integral part of construction practice and not some esoteric academic exercise.
In his paper on the mechanism of landslides, Terzaghi (1950, p. 91) made the comment:water in contact with many common minerals, such as quartz, acts as an anti-lubricant and not as a lubricant.
Although this was known in 1950, to this day there are still reports in the media and even in some scientific articles about landslides being caused by ‘water lubrication’. Some lessons, it seems, are never learnt. Reading the whole paper, it becomes apparent how advanced the understanding of landslide mechanisms was 70 years ago. It also appears to be the case that since 1950 lessons about landslide mechanisms and the effects that slope instability can have on construction have had to be re-learnt many times.
In terms of lessons not being learnt, the paper by McConnell et al. (1950) shows that alkali–aggregate reactivity (AAR) is not a new phenomenon. Their paper indicates that it was first recognized as an issue in Southern California in 1938 following the rapid and intense deterioration of concrete structures that had been identified over the previous 20 years. Further work during the 1940s (e.g. Hansen 1944) revealed the nature of the problem. However, damage to UK structures caused by the process labelled in the media ‘concrete cancer’ can be traced through to the 1990s, as illustrated in the article by Bevan (2007) on the South Wales Millennium Stadium completed in 1999, which was affected by AAR.
The Berkey Volume is full of examples of the application of geology to all aspects of civil engineering practice and provides advice that remains applicable to the present day. It is the ideal benchmark against which to measure the advances that have occurred since 1950. There have been a number of useful interim benchmarks that track the progress of the discipline in the USA, with a particular highlight being The Heritage of Engineering Geology: The First 100 Years (Kiersch 1991b). Published by the Geological Society of America, this 600+ pages volume contains a wealth of information and a superb collection of case studies. Most usefully, it contains many examples of where things went wrong. These days the threat of litigation has effectively stopped such case studies being published, thus the lessons from recent failures will never be learnt and similar mistakes will continue to be made. In the UK the best way to track the progress of engineering geology is through the articles in the Quarterly Journal of Engineering Geology and Hydrogeology (QJEGH, first published in 1967); the Glossop lecture series (starting with Fookes 1997), most of which have been published in QJEGH; the Engineering Geology Special Publications of the Geological Society of London (EGSPs); and the various working party reports of the Engineering Group of the Geological Society (e.g. Walker 2012), which have all been published either in QJEGH or as EGSPs. However, perhaps the most useful global ‘golden spike’ for the present state of the art is the Encyclopedia of Engineering Geology edited by Bobrowsky & Marker (2018). It is fascinating to compare the contents of this encyclopaedia with the Berkey Volume as it shows how far many of the facets of engineering geology have progressed. Identifying some of the highlights in this progression is the purpose of the rest of this paper.
Site investigation: initial stages
Any evaluation of advances in engineering geology in the UK since 1950 must start with site investigation. Hatheway (2002) stated that ‘site characterisation’ is the raison d’être for engineering geology and site investigation lies at the heart of this process. In this section the initial stages of the site investigation are reviewed, encompassing the developments in desk studies, remote sensing and field mapping.
Desk studies
The first step in any site investigation is the desk study. Since 1950 this has changed out of all recognition with the advent of information technology (IT) associated with the internet and electronic publications that provide immediate access to enormous quantities of data. This represents an incredible step forward from the old approach, which required physical visits to libraries, newspaper archives, museums, etc. There can be no excuses these days for not carrying out a comprehensive desk study that brings together all relevant information about a site of interest. However, based on some of the observed practice it is necessary to issue some words of warning that that are particularly relevant in the context of the EGGS Cambridge Conference.
It is necessary to ensure any literature searches differentiate between fact and fiction. There are millions of websites that contain information of relevance to environmental and engineering geology; however, not all can be trusted to provide accurate data. For example, there are websites that attempt to give credence to Bishop Ussher's view that the Earth was created on 23 October 4004 BC, or that the Earth is flat. Accessing sites that can be trusted is vital and the most suitable are listed below.
National, regional and local government and government departments. All aspects of development planning stem from government decisions and the documentation will be available on government websites. There will also be departments or offices within the government that have special responsibilities, such as the Department for Environment, Food and Rural Affairs (DEFRA) in the UK.
Government support agencies. In all countries there are government agencies that are nominally independent of the government and some may also undertake commercial work. These agencies set guidelines, prepare codes of practice and lay down standards that will be referred to in contracts for mining, environmental or construction work. In the USA an example is the Environmental Protection Agency (EPA) and in the UK the equivalent would be the Environment Agency, which is sponsored by DEFRA.
Standards organizations. A key element in environmental and engineering geology is the adoption of ‘standards’ that define the methods for carrying out work. These standards are often internationally recognized and form a key component of commercial contracts to ensure work is carried out in a way that is fully compliant with a specification. BSI Group (the British Standards Institution) is the national standards body for the UK, although it also operates internationally. There is also the International Organization for Standardization (ISO), and the geotechnical standards relevant to the UK carry both a BS and an ISO kitemark. A full discussion on these UK and European standards has been given by Norbury (2017). In the USA there is ASTM International (formerly the American Society for Testing and Materials), which has over 12 000 standards that are used globally. The military may also be a source of standards; for example, the US Army Corps of Engineers produces documents on codes of practice to be used in areas of contaminated land and for geotechnical investigations. Many of the standards developed by these various groups fall within the field of environmental and engineering geology, and failure to use the standards correctly can have legal implications.
National and regional geological surveys, soil surveys and conservation services. These surveys can be found in countries throughout the world. For example, the United States Geological Survey (USGS) provides a vast amount of free information and high-quality data not just for the USA but globally. The British Geological Survey (BGS) takes a similar role in the UK. In the USA each of the states also has its own geological survey. National and regional geological survey websites should be the first call in any desk studies.
National, regional and local museums, and local libraries. In the UK, the British Museum and the Natural History Museum hold a wealth of data, although in common with most museums not all the information is available through the websites, and site visits and often special permissions are required to access it. Local museums, and local libraries, can be particularly useful sources for information about prior use of brownfield sites in their region.
National libraries and institutions. There are many examples of these types of institution. In the USA the Smithsonian Institution, which was established in 1846, is the world's largest complex of museums and research centres and is administered by the US Government. In the UK, the British Library in London describes itself as the largest library in the world in terms of the number of items catalogued. In Australia CSIRO (formerly the Commonwealth Scientific and Industry Research Organisation) is a more active research institution and is Australia's largest patent holder. In Hong Kong the Geotechnical Engineering Office (GEO) is a government-based organization that has led and sponsored extensive research into ground conditions within the area and provides comprehensive and freely available reports. NASA would fall under this category and provides an enormous amount of free remote sensing data. These types of institutions can be relied on to provide access to accurate and up-to-date information, as well as holding long data archives.
National parks, geoparks, World Heritage Sites, etc. This is a broad category as every country has its own designation for locations that have been identified as having special scientific merit. However, these all have websites that are excellent sources of information and often hold spectacular images. The US National Parks Service deserves special mention in this respect.
International bodies. United Nations based bodies such as UNESCO, UNISDR, FAO, UNEP and WHO are important sources of both data and long-term plans for improving global conditions (e.g. issues of sustainability, climate change, human rights, etc). The UN supports groups such as the Intergovernmental Panel on Climate Change (IPCC), which is an international group set up by the World Meteorological Organization (WMO) and the United Nations Environment Programme (UNEP) to advise on and monitor the latest research pertaining to global climate change. The European Commission has also supported many research programmes that have provided substantial funding to member countries, much of which has been geared towards societal improvement. Reports from these European Union projects are readily available.
University repositories. Increasingly universities around the world have digital repositories where publications by staff can be accessed.
Learned and professional bodies. Around the world there are institutions such as the International Society for Engineering Geology and the Environment (IAEG), Geological Society of London (GSL), Institution of Civil Engineers (ICE), Institute of Materials Minerals and Mining (IOM3), the Geological Society of America (GSA), the American Institute of Professional Geologists (AIPG), the Australian Geomechanics Society (AGS), the Canadian Geotechnical Society, etc. All such institutions have their own codes of ethics that ensure material they and their members publish is of the highest scientific standard. In addition, many such bodies have their own publishing houses, which can be relied upon for providing state-of-the-art and peer-reviewed work.
Company websites. Company websites can usually be trusted to provide accurate and up-to-date information in countries where laws against incorrect and inappropriate advertising are enforced. Civil engineering construction companies are a particularly useful source of case studies, as indeed are local museums and libraries.
National and regional newspaper archives. Although newspapers tend to hold their own political views and the standard of scientific writing is often disappointing, they do record the occurrence of natural and human-made disasters fairly accurately. These reports can be invaluable when trying to establish the regularity of occurrence of geohazards and provide useful information on the effectiveness of disaster planning and recovery plans.
It should be remembered that the internet will remain only a partial source of information until comprehensive archives of data from all previous site investigations are available. Many of these ‘grey’ data are locked away in client files and remain inaccessible, some because they are available only as hard copy and are not readily recoverable or transferable but others because of issues surrounding copyright and client confidentiality.
Publications that are more than 10 years old do have legitimacy and should not be ignored. Some older guidance documents (although current) have been removed from government websites but many are located on the CL:AIRE (2019) website.
The scope of a desk study was described by Clayton & Smith (2013), who quoted AGS (2006) that a desk study ‘is often considered to be the most cost-effective element of the investigation’. It is axiomatic that as much prior information as possible about a site is collected beforehand, so any ground investigations can be focused on priority areas, such as those lacking data or that are particularly problematic.
Remote sensing
Another element of desk studies that has developed beyond all recognition since the Berkey Volume is the nature, availability and scope of remote sensing. Remote sensing for engineering projects in 1950 involved using stereographic pairs of black and white aerial photographs. Interpretation (API) was carried out manually on overlays that were then transferred to spatially correct maps and plans. The advent of satellite imagery from the 1970s onwards has transformed the amount and quality of data that can be obtained from remote sensing. Multispectral (MSS) and hyperspectral scanners (HSS) mounted on satellite platforms allowed the collection of data over a much larger part of the electromagnetic spectrum and at high resolutions.
The most recent relatively cheap high-resolution remote sensing technique is the use of airborne drones. With the capability of carrying digital cameras providing data that can be geo-referenced and enhanced using a range of easily obtainable software systems, these are capable of collecting large-scale images of sites that are of direct value to engineering, environmental and mining projects. As an example, Figure 2 shows a drone image of a landslide in SE Spain that lies on the outside of a meander bend. This image provides data that allow an interpretation of the nature and cause of the landslide to be undertaken.
Maleguica landslide in SE Spain. Image created by taking overlapping vertical images using a DJI Phantom 3 Professional drone. The images have been stitched together using AGISsoft Photoscan. Resolution is c. 20 cm (image produced by M. Stokes, SoGEES, University of Plymouth and used with permission).
It is not just the passive satellite receivers that have changed; a range of active scanning systems mounted on satellites and aircraft have emerged. LiDAR (light detection and ranging) is one of the most important as it can provide spatially corrected high-resolution ground images for interpretation even if the terrain is covered in dense forest. Increasingly, countries are providing LiDAR data as an open access resource and Figure 3 shows a LiDAR image of the same landslide as shown in Figure 2. Using contour colouring highlights the shape of the landslide with the backscar and accumulation debris being clearly delineated. Combining the LiDAR and drone data allows digital elevation models (DEMs) to be constructed over which a range of Earth science data can be draped to produce digital terrain models (DTMs).
Maleguica landslide in SE Spain produced from publicly available Spanish Instituto Geografico Nacional LiDAR data; resolution for 1 pixel is 1 m horizontal (image produced by M. Stokes, SoGEES, University of Plymouth and used with permission).
Another useful active scanning satellite system is InSAR (interferometric synthetic aperture radar). This scanner can map and monitor surface deformation and is capable of detecting deformation of the ground surface to millimetre accuracy. Repeated measurements over days or even decades mean it is now possible to monitor landslide or subsidence movements from space.
The wealth of remote sensing techniques and readily available data has led to an increase in their use in the initial stages of a site investigation. However, information derived by remote sensing still needs to be checked by the process known as ‘ground truthing’. This can be achieved only by field mapping.
Field mapping
Back in the 1970s famous practising engineering geologists such as Dearman & Fookes (1974) and Clark & Johnson (1975) emphasized the importance of engineering geological and geotechnical mapping to provide a spatial framework for designing and interpreting ground investigations. Brunsden et al. (1975) showed how mapping the geomorphology could provide information on natural hazards, present-day processes and relict landforms that was directly relevant to interpreting the ground conditions for engineering projects. The value of mapping in engineering practice was summarized by Dearman (1991) and Griffiths (2002). All this mapping was based on fieldwork, although it drew heavily on the interpretation of remote sensing data. However, looking at the last decade of the UK literature in engineering geology there are fewer examples of actual field mapping as a component of site investigation, and that is concerning. The UK led the world in field mapping for engineering projects and the fear is that the skill is being lost (Griffiths 2014; Privett 2019).
Figure 4a is an example of some large-scale geomorphological mapping on part of the Undercliff landslide complex on the Isle of Wight from Griffiths et al. (2015). There were no subsurface data available at the time of the mapping but there was literature on other parts of the Undercliff that was used in conjunction with field mapping to allow a cross-section of the landslide complex to be compiled (Fig. 4b). This took two person-days on-site and one person-day for writing up the report. The report was used as the basis for designing a ground investigation to stabilize the coastal road. By any measure this was a very cost-effective exercise.
(a) Geomorphological map and (b) cross-section of the Binnel Bay landslide (reproduced from Griffiths et al. 2015, with permission from the Geological Society of London).
As one of the leading exponents of the art Hearn (2017) demonstrated the continuing importance of maintaining these field mapping skills, but the list of UK practitioners who are still doing work of this type is disappointingly short and the names on the active list are getting worryingly ‘mature’. This is one example of a sub-discipline of engineering geology that did advance significantly but now appears to be regressing.
Site investigation: the ground investigation (GI)
At the time of the Berkey Volume the GI would have involved trial pits and various types of drilling. In the UK there would have been shell-and-auger (i.e. light cable percussion), rotary drilling using water flush with both open-hole and some coring probably with single core barrels. In situ testing in boreholes was mainly limited to the standard penetration test (SPT), first introduced in 1902 as a sampling technique in soils (Clayton et al. 1995). Geophysical techniques were available, but the methods were still being developed. Since then drilling has progressed through the application of different flush media (air, foam, mist and polymers) and the use of double and triple core barrels to aid core recovery. In situ testing (Mayne 2006) and geophysical techniques (McDowell et al. 2002) have both expanded and developed significantly since 1950. However, in some cases there has been a divergence in the use of some new methods between the onshore and offshore ground investigation industries. For example, offshore there has been widespread acceptance of the cone penetration test (CPT) for in situ testing and geophysics as a ground investigation technique, but onshore there does not appear to have been the same level of application. This is explored further below.
Usefulness of various in situ tests
According to Simons et al. (2002, p. 246), in the presentation of his paper at an international conference Mayne (2001) asked the question: ‘Is it time to retire the SPT?’ It was Terzaghi at the 1947 Texas Soil Mechanics Conference who first recognized that the blow count of an SPT could be used to obtain soil consistency or density data (Fletcher 1965). But 66 years later in the July 2013 edition of the on-line journal Geotechnica there was a report of a recent geotechnical meeting where it was stated: ‘Discussion moved on to consider the use of SPT for design. It would seem that this is now the most commonly used test to determine ground strength and hence bearing pressure’ (Anonymous 2013). It is doubtful that Terzaghi would have been impressed by the continued use of the SPT for design work given the developments in CPT technology since 1947. Table 2 is based on Robertson & Cabal (2015) and compares the value of the data obtained from a range of in situ tests including SPT and various types of CPT including the piezocone (CPTu) and the seismic cone (SCPTu). There are also data on the flat plate dilatometer (DMT) and the seismic dilatometer (SDMT). Comparing the CPT with the SPT shows that the CPT provides high-quality data for a much wider range of ground conditions.
The applicability and usefulness of some in situ penetrometer or direct push tests (based on Robertson & Cabal 2015)
The difference between CPT and SPT data was highlighted in a paper by a Japanese team working in the Mekong River Delta in Vietnam (Hoang et al. 2016) (Fig. 5). They showed the results from different techniques in an investigation of the geotechnical properties of a late Pleistocene to Holocene deltaic sediment sequence. In Figure 5 the geological log on the left in column (a) was compiled using continuous sampling with a hydraulic thin-walled sampler. The soil-behavior-type classification in column (b) is an interpretation of the piezocone results shown in columns (c)–(h) using charts such as those of Robertson & Cabal (2015). Column (i) on the right gives the SPT results. Figure 5 shows that if a simplified interpretation of ground conditions is all that is wanted then an SPT will suffice, but if an accurate record of the actual soil types and their geotechnical properties is needed the CPT piezocone provides much better results.
Comparison of logs obtained from various in situ tests obtained for a site in the Mekong Delta, Vietnam (from Hoang et al. 2016; open access paper and reproduced under creative commons license CC BY-NC-ND-4.0).
Geophysics for construction engineering
In 1950 geophysics in ground investigation was in its infancy, although it was probably first developed in the early 1920s (McDowell et al. 2002). Most developments of the techniques have been within other industrial sectors, notably in petroleum exploration and mining. The offshore hydrocarbons industry, having experience in geophysical applications for exploration during the 1950s and 1960s, readily made widespread use of geophysical techniques in the investigation of seabed and shallow subsurface conditions for offshore structures such as oil platforms and submarine pipelines. However, the onshore ground investigation industry has been more reluctant to embrace the techniques (Griffiths & Culshaw 2004) and has preferred to concentrate on the use of exploratory holes. This may be partially explained by the comment of Clayton & Smith (2013, p. 27): ‘Geophysical investigations have a high failure rate under unfavorable circumstances’. Nevertheless, Gunn (2017) reviewed some 140 papers from the 50 years of the QJEGH (and its forerunner the QJEG) that illustrated the development and use of geophysical techniques for ground investigation over the previous 50 years. Sixty per cent of the contributions involved seismic, electrical resistivity and thermal methods. The EGGS Working Party report by McDowell et al. (2002) reviewed the full range of geophysical techniques that can be applied in engineering practice and a summary of the methods has been provided by Tuckwell (2018). Geophysical techniques have advanced significantly since the Berkey Volume and it remains a mystery to this author why too many engineering geologists are willing to ignore techniques that are perfect for filling in the gaps in subsurface information between exploratory holes as well as identifying anomalies requiring further investigation. Hopefully, as the large number of positive examples make their way into the scientific literature, geophysical techniques will become increasingly accepted as a key onshore ground investigation tool.
Site investigation: the cost
Whereas most site investigation (SI) techniques have progressed significantly since the Berkey Volume, even if they are not all being used, an area that has regressed is in persuading some clients that money spent on a good SI will reduce costs in the long term. This was highlighted by the image shown in Figure 6 that was circulated recently by Ian Clarke on LinkedIn, and was a point made strongly by Grainger (2018) of the British Drilling Association with respect to procurement for ground investigations. As indicated, clients have the options of a cheap, fast or good ground investigation, with any two of these choices being possible but not all three. So, although there are the techniques to improve the process, how can clients be persuaded to pay for a good SI or GI rather than just taking the cheapest quote? One facet of this is that it should be recognized that clients will get away with a cheap SI on ‘forgiving’ sites (expression from Hencher 2012, p. 116) with no particularly hazardous conditions but not on ‘unforgiving’ sites (Hencher 2012, p. 116) with inherently difficult ground conditions. Perhaps clients treat their approach to procuring a cheap SI as a calculated risk and until they suffer a major financial or public relations disaster resulting from an inadequate SI, they will continue to take the cheaper options. But, as Grainger (2018) suggested, it is doubtful these clients really understand the level of risk they are accepting until they face the consequences of a failure and, even then, one wonders if they will be willing to accept the blame and liability?
Venn diagram showing a client's choices for a site or ground investigation.
Communications and data management
Perhaps the biggest advances both in society and engineering geology since the Berkey Volume have been in communications, information technology (IT) and data management. Back in 1950 the computing power now available just on mobile phones could not have been imagined. However, this has created its own novel problems and the management and interpretation of data has become an industry in itself. IT has been addressed above in relation to desk studies; the issues arising from better communications, data management and creating a ground model are discussed below.
Communications
Early images of field geologists show, predominantly, men out in the wilds and a long way from their head office. In the world of engineering geology, until the widespread availability of mobile phones in the late 1990s, any engineering geologist who was on-site in the UK was essentially on their own, apart from the odd phone call from a public phone booth or hotel (if they were lucky enough to be staying in one) to their line manager. The engineering geologist on-site kept a detailed hardcopy site diary and if problems arose had to deal with them by themselves, learning from the experience. Thus, from the time of the Berkey Volume until the late 1990s the site experience of engineering geologists in the UK was very similar. The advent of mobile and satellite phones, laptop computers and emails has changed this image beyond recognition. Now if problems arise phone calls can be made to line managers straightaway. At least one UK company is also offering an app for smartphone or tablet that allows the user to interact with desk study information and add geo-referenced notes, photos, etc. that can be viewed by a manager back in the office in real time (Envirocheck 2019). One concern is that this immediate access can lead to the temptation to micro-manage the engineering geologists who are on-site. There will be many early career engineering geologists who have thought, ‘I wish my line manager would stop phoning and let me get on with the job!’ Although the opportunity provided by mobile phones may have resulted in some deterioration in the learning experience for early career engineering geologists, rapid communications will almost certainly have led to better ground investigations with fewer delays. Although more mature engineering geologists may reflect on some of the ‘white-knuckle rides’ during their early career experiences on-site with a degree of rose-tinted hindsight, better ground investigations, effective risk assessment and improved standards of health and safety resulting from modern communications must be lauded.
Data management
Extensive site investigations generate vast amounts of data, and in common with all facets of geology, these data are spatially related (‘geolocated’). From the time of the Berkey Volume until the early 1970s these data will have been collated, compiled and analysed by teams of engineering geologists who would produce hardcopy reports where interpretations and data were typed up with graphs, maps and diagrams drawn by specialist cartographers from hand-drawn originals. This changed once readily accessible computing power became available. Reports were word-processed, data were loaded into databases and spreadsheets to be analysed, and maps, plans and diagrams could be produced using computer-aided drafting (CAD) systems. Initially, this still tended to result in hardcopy reports where data were not fully integrated, but this changed with the development of geographical information systems (GIS), specialist borehole data handling software (e.g. AGS 2012) and a preference for electronic reports that could be made available to all users. Komac (2018) wrote that the term GIS describes ‘any information system that integrates, stores, edits, analyses, shares, and displays geographically defined information’. Although Turner (2003) advocated the use of the term GeoScientific Information Systems (GSIS) for GIS that involved geoscience data interpolation and extrapolation procedures and interactive data manipulation, the term GIS has now been accepted to describe the spatial database systems that are one of the most widely adopted approaches in engineering geological data management on large complex construction projects. However, looking to the future, a critical aspect of any GIS for use by engineering geologists is the need to ensure it is able to integrate data from other systems, notably some of the industrial standards for recording borehole data such as the AGS data format (Bland et al. 2014).
Another facet of data management that has emerged is building information modelling (BIM). This is the process of creating and managing data on a construction project across the whole project lifecycle (Kensec 2014). Through BIM, the construction industry is undergoing its very own digital revolution. BIM is a way of working and creates value from the combined efforts of people, process and technology. The key output is the building information model, the digital description of every aspect of the built asset. Creating a digital building information model allows those who interact with the infrastructure to optimize their actions, resulting in a greater whole-life value for the asset. However, there continues to be a need to ensure all the data held in these various digital systems are integrated with other ground investigation data.
Ground model
A key element of data management for engineering geologists is the construction of a ground model (Fookes 1997), which is now regarded as a fundamental component of a site investigation. Although the basic idea has been around since the Berkey Volume, as can be seen in the examples of cross-sections for dam sites given by Burwell & Moneymaker (1950), carrying out this process has been revolutionized by the computing power now available. Parry et al. (2014) defined three types of ground model.
Conceptual
Conceptual models are essentially qualitative in nature and illustrate the key features of a geological situation and the processes active in that environment. The importance of conceptual ground models has been a major focus of recent EGGS Working Parties (Walker 2012; Griffiths & Martin 2017) and is a key element of an excellent study of Quaternary landscapes in the UK by Booth et al. (2015).
Observational (see Culshaw 2005)
These are scaled-down versions of ground conditions at specific sites based on actual data. These are created when ground investigation data are obtained and, based on the initial conceptual models, the best estimate of ground conditions is produced as two-, three- and four-dimensional observation models. These models are often created on GIS platforms.
Analytical
These are representations of reality using mathematical formulae, different media or schematics. Many of the geotechnical models used to calculate the stability of foundations or slopes fall into this category (e.g. Stead & Coggan 2012).
Conceptual ground models provide the first step in building a site-specific observational ground model. Conceptual models characterize the general nature of the ground conditions, the likely geotechnical issues that will need to be addressed, the location of any useful resources and the likelihood of any particular geohazards. Effectively, they can be considered a checklist of the types of things that should be looked for in the subsequent ground investigations. However, for detailed engineering design these conceptual models must lead to the creation of observational and analytical models that fully characterize the ground conditions at a proposed construction site. Preparation of these models represents the accepted current approach to data management for engineering projects in the UK.
Health and safety
The injury and loss of life on construction projects has long been a concern. During the construction of the Hoover Dam in the USA in 1931–1936 the official death toll amongst workers was 96. Even on the Channel Tunnel, which opened in 1994, 10 workers were killed, although given a workforce of over 13 000 that is a very low percentage. Nevertheless, the construction industry is potentially hazardous and major efforts have been made to reduce the risk to workers in the UK, by government through the Health and Safety Executive created in 1974, by the actions of professional bodies, and by improved practice in all civil and ground engineering related companies. There is extensive legislation and guidance in place to ensure workers on-site are protected and effective risk assessments are carried out before any work is undertaken. Engineering geologists have benefited from all these efforts and an example of the work of a professional organization is provided by the British Drilling Association (2015) Health & Safety Manual for Land Drilling, which was the culmination of a series of safety manuals on all aspects of ground investigation. However, it should be remembered that the first successful prosecution under the UK 2007 Corporate Manslaughter Act was of Cotswold Geotechnical Holdings, which was charged with unlawfully killing an early career engineering geologist who had been working alone in an unsupported 3.8 m deep trench that collapsed (Reed 2011).
Without doubt, safety on-site for engineering geologists has improved since 1950 and quite rightly. Some of the lax and dangerous practices highlighted by the Cotswold Geotechnical Holdings case are recognized as completely unacceptable. Safety, however, remains as much a personal as a corporate responsibility and it is an obligation on all professionals to speak out whenever they identify unsafe practices.
Professionalism
Under the overall heading of professionalism, there are two elements that have changed dramatically over the past 70 years: the professional recognition of practising engineering geologists in the UK, and the development of national and international standards for site investigation.
Status recognition of the profession
In 1950 both in the USA, based on the Berkey Volume, and in UK the concept of an ‘engineering geologist’ requiring a ‘professional’ qualification does not appear to have been a high priority. Suitably experienced geologists would be used on civil engineering projects as required, working alongside civil and geotechnical engineers. However, in the UK over the following 30 years the concept of ‘chartered status’ became an increasing requirement, notably when the Engineering Council was established in 1981 with the responsibility of licensing member organizations, including the Institution of Civil Engineers (ICE) and IMM (as it was then), to be able to award professional titles such as CEng. Just after this the Institution of Geologists (IG, originally part of the Geological Society of London (GSL)) sought to establish the title Chartered Geologist (CGeol) as the geologist's professional equivalent of CEng. With the reunification of the IG and the GSL at the start of the 1990s the title CGeol became a core award the GSL could confer on appropriately qualified geologists under its own Royal Charter. Since then, work by Ground Forum (GF), GSL, ICE, IOM3 and the British Geotechnical Association (BGA) facilitated the establishment of the register of ground engineering professionals (RoGEP) that, in 2011, finally put CGeol and CEng on an equivalent status for appropriately qualified individuals working in the civil engineering industry. For engineering geologists, it is only chartered geologists who can submit a peer-reviewed application to be placed on the register and their status continues to be recognized only by the production of a recorded programme of continuing professional development (CPD). However, as of September 2018 there are still fewer than 1000 people listed on the RoGEP in the UK. Part of the problem is that clients for ground engineering projects have still not fully embraced the need to appoint a RoGEP listed professional to manage activities such as ground investigations, and this may also be a product of the preference for some clients to always choose the cheapest option (see above discussion).
Status recognition remains a work in progress in the UK, a theme that is also encountered in the USA (Tepel 2004). All the elements are in place but there remains a great deal to do to promote the importance of appointing professionally qualified staff to undertake projects in engineering geology.
International standards for site investigation
Norbury (2017), in his 17th Glossop lecture, provided a summary of the development and importance of national and international standards to define best practice in site investigations, including accepted methods for describing soils and rocks for engineering purposes. Without doubt the development of such standards by internationally recognized bodies is one of the most important features of the modern practice of engineering geology. By 1952 in the USA, just after the Berkey Volume was published, the main system for classifying soils was accepted as the Unified Soil Classification System. In the UK the first publication that defined the standards of a site investigation, and included information on soil and rock description, was BS CP 2001:1957 (BSI 1957). The latest standards for the UK are described in a series of publications by the BSI (Norbury 2015, 2017) that meet the requirements of the ISO based in Geneva. These standards define best practice for all aspects of a site investigation and ensure all such work is carried out to a common level of quality using terminology that is accepted and recognized by all engineering geologists. The importance of these standards cannot be overstated.
Conclusions and the future
There will be debate over the most important advances in engineering geology in the UK as measured against the baseline of the 1950 Berkey Volume, but in Table 3 this author's suggestions for the most significant developments are listed. Whatever any one individual regards as the most important, nobody can deny there has been an enormous leap forward in the subject over the past nearly 70 years. Some of these developments have been driven by industrial needs, such as seeking better core recovery leading to the use of different flush media and triple core barrels, or the requirement to use non-invasive techniques of investigation resulting in significance advances in mapping, remote sensing and geophysical techniques. However, many are global societal developments in technology that have been found to be of value in engineering geology, and here computing power and communications stand out. However, one significant question does emerge: the techniques are there but are they all being used and used effectively? In site investigation, surely the core activity for engineering geology, this comes back down to cost. But it pays to remember the old adage, ‘you pay for a ground investigation whether you have one or not’ (Waltham 2009, p. 42), as a lack of data on ground conditions will inevitably lead to over-conservative design, expensive changes to design during construction, or possibly litigation following a failure.
Author's suggestions for the most significant developments in engineering geology in the UK since 1950
Looking to the future there will be both new and a continuation of existing challenges for engineering geologists to deal with. The new topics that will be emerging in the future may have an increasing environmental emphasis, in particular those relating to climate change (Nathanail & Banks 2009), and the need to reduce our carbon footprint including seeking out renewable energy sources. Issues surrounding waste disposal and ground contamination (Nathanail 2009, 2013) will not go away, and there will be increasing emphasis on reuse, recycle and restore. It will be interesting to see the development of geoforensics (Pirrie et al. 2013), notably in relation to environmental issues, and if geoscientists can improve the way they communicate environmental geoscience to both the general public and lawmakers (Liverman et al. 2008; Lee 2015).
It is also now recognized that society is facing the next industrial revolution, labelled ‘Industry 4.0’, which covers the current trend of automation and data exchange in manufacturing technologies. This includes cyber–physical systems, the ‘internet of things’, cloud computing and cognitive computing (Marr 2018). Industry 4.0 creates what has been called a ‘smart factory’ and it will be interesting to see what effect this has on data handling methods in engineering geology and geotechnics.
Finally, there is the next generation of engineering geologists to train. Here it is necessary to sound a few notes of caution because in the UK a number of the specialist MSc programmes have closed as funding disappears; research councils seem reluctant to support research in the discipline; engineering geologists have been criticized for lacking the basic mathematics to engage with complex deterministic and probabilistic ground models used in design by geotechnical and civil engineers; companies are facing problems in mentoring early career staff partly thanks to ‘value engineering’; and there is the difficulty of persuading capable students into a career in engineering geology when competing jobs seem to be paying more. Knill (2003) raised these and many other issues in a wide-ranging debate in the first Hans Cloos Lecture for IAEG on the core values of engineering geology. Therefore, all engineering geologists have a responsibility to promote their discipline as both a wonderful career and one that is vital for ensuring safe, economic and sustainable construction and development in a modern society. Tepel (2002) labelled this ‘stewardship’, which describes it perfectly, and it is a responsibility we must take seriously if engineering geology is to thrive in the future.
Acknowledgements
This paper is based on over 40 years’ experience in engineering geology and geomorphology and draws on the innumerable encounters and conversations with my professional colleagues over this considerable time period. My gratitude goes to all of them, but I owe particular thanks to P. Fookes and D. Brunsden, who got me started in the profession back in 1976. I also want to thank the reviewers of this paper for their many helpful suggestions.
Funding
This research received no specific grant from any funding agency in the public, commercial, or not-for-profit sectors.
Scientific editing by Joel Smethurst; Phil Renforth
- © 2019 The Author(s). Published by The Geological Society of London. All rights reserved