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Rock Solid Defense for Accidental Pond Drowning

Andrew J. Davidoff, Ph.D., P.G., Geology, Geophysics, and Earth Science Expert

Case Summary: The incident in question involves the drowning death of an older adult found in a pond behind the family residence. The discovery was made by a pond management company employee, who initially mistook the body for a floating object. The police treated the investigation as a potential homicide. An autopsy later revealed that the cause of death was drowning, and the incident was ruled accidental. The deceased was visiting their family, whose residence opened directly onto the pond.

The primary issue revolves around whether the rocks surrounding the pond contributed to the incident. The plaintiff claimed that the rocks were slippery, leading to the deceased’s fall, head injury, and subsequent drowning. The scope of the requested work was to scientifically analyze the rocks to determine if they were indeed slippery and thus contributed to the accident.

Expert Analysis: The analysis began with a thorough review of case-specific documents, including the summons and complaint, various discovery documents, police investigation reports, crime scene photographs, and expert reports from the plaintiff.

Crime scene photographs were of sufficient resolution to conduct a detailed analysis of the properties of the rocks in the area where the victim fell. The analysis focused on evaluating the photographs for the structure, texture, and color of the rocks.

Careful inspection of the photographs under high magnification indicated the rocks had a rugose or rough texture. Many of the rocks also displayed faint small-scale layering. The small-scale layering is strong evidence of sedimentary deposition, while the rough texture is an indicator of sand-size grains. The reddish-brown color of the rocks is an indicator of hematite cement, common in sandstones.

The rocks in the photo below are sandstones, similar to those around the pond discussed. They display a rough texture, distinct sedimentary layering, and reddish-brown coloring indicative of hematite cement.

A pile of red rocks is sitting on the ground.

Based on the above analysis, the rocks in the vicinity of the pond were identified as medium- to coarse-grained sandstone. The presence of hematite cement and the visible sedimentary structures further confirmed this identification.

Anything with a coefficient of friction greater than 0.5 is considered slip resistant. Sandstones are documented to have a coefficient of friction between 0.71 and 0.85. The coefficient of sandstones is significantly greater than 0.5, indicating that they are slip resistant.

Based on the scientific analysis, it was concluded that the rocks around the pond were not slippery, and thus, did not contribute to the deceased’s fall and subsequent drowning. The incident was likely a tragic accident unrelated to the condition of the rocks.

Result: The case was resolved prior to trial.

Contact A.J. Davidoff LLC at (281) 771-8916 for your geologic, geophysical, and subsurface expert needs or visit www.forensicDJS.com for additional areas of expertise. 

By Andrew J. Davidoff, Ph.D., P.G. November 8, 2024
Case Summary One of the first things an oil and gas company must do before they can drill a well is to obtain the mineral rights for the land they want to drill on. The most common way to do this is to lease the mineral rights to the land. These leases come with certain unwritten legal or hidden obligations, known in the legal world as “implied covenants.” Oil and gas leases contain several implied covenants. One of them is known as the “Duty to Develop.” This refers to the obligation of an Oil and Gas Company (the lessee) to make reasonable efforts to explore and develop an oil and gas lease. Whether or not an oil and gas company has lived up to its obligation to develop a lease responsibly may become a matter of dispute and sometimes ends up in the courts. Understanding the subsurface geology is often critical in determining whether a company has met its obligations. The question often comes down to whether a company can profit from additional drilling or other development activities. Answering this question is, at least in part, frequently dependent upon the potential quantity of oil and/or gas in the subsurface. These questions require the expertise of geologists and often additional subsurface professionals such as geophysicists, petrophysicists, reservoir engineers, and others. The following provides an example in which an operator was found to have breached their obligations to make reasonable efforts to explore and develop oil and gas in a lease and the role geology played in the case. The case went to court in the 1980s, but its origins can be traced back to the 1930s when a major oil and gas company leased a 10,000-acre tract of land along the onshore Texas Gulf Coast. The company used seismic reflection technology to explore for oil and gas on the lease. The use of seismic reflection data in oil and gas exploration is common and standard operating procedure today, but in the 1930’s, it was leading-edge technology. The use of seismic enabled the discovery of oil and gas in a sandstone layer in a rock unit called the Frio Formation. The discovery was made in the early 1940s. Over the next decade, the company found three more oil and gas-bearing sandstone layers in the Frio Formation. By the time the case went to trial, the company had drilled 64 wells and acquired an additional 13 seismic surveys. The field covered an area of over 1,100 acres. It had produced over 100 million barrels of oil, over 100 billion cubic feet of gas, and over 50,000 barrels of condensate, with royalties providing an average income of $10,000 per day. At the time of the trial, 37 wells were still producing. However, the remaining 8,900 acres of the 10,000-acre remained unexplored and undeveloped. Fields along the Texas Gulf Coast were also known to produce hydrocarbons from slightly deeper and older sandstones in the Vicksburg Formation. The case hinged on the question of whether the operator had fulfilled its obligation to explore the remaining 8,900 acres and test the potential of the Vicksburg Formation. Expert Analysis The Operator claimed there was only one structure and one formation with sufficient porosity and permeability to trap and produce hydrocarbons. The landowner (the lessor) challenged this claim and hired a geologist to review the subsurface data. The geologist for the lessor reviewed the data across the field and concluded that the remaining 8,900 acres of land could contain additional oil and gas accumulations. They also concluded that oil could be present not only in sandstones of the Frio Formation but also in a deeper formation called the Vicksburg. The jury was tasked with determining whether the Oil and Gas Company had acted reasonably in exploring and developing the lease. The answer to this question required the jury to learn about the geology in the area, how the oil and gas became trapped in the rocks, and the tools used by geologists and geophysics to understand the subsurface. The subsurface along the Texas Gulf Coast is dominated by sandstones and shales deposited by ancient rivers and in deltas, beaches, barrier islands, and marshes. The sandstones form porous and permeable layers that can both store oil and gas and through which oil and gas can move or migrate. These layers are often called reservoir rocks. Shales form impermeable layers through which oil and gas cannot move, often called seals. Oil fields are formed when reservoir rocks, seals, and subsurface structures combine in such a way as to create a feature (called a trap) into which oil can migrate and be stored for 10s and even 100s of millions of years. There are many different types of traps in which hydrocarbons can accumulate. One of the most common is the anticline. An anticline resembles a hill or an inverted bowl. Oil or gas will migrate upward through porous rocks and become trapped at the crest of the anticline (Figure 1a). The oil industry aims to find hydrocarbons trapped in the subsurface that can be produced at a profit. To do this, the oil and gas industry collects and analyses vast quantities of subsurface geologic and geophysical data. These data are divided into two broad categories: well data and seismic data. [1] Well data is information collected from the well bore, that is the hole in the ground created by the drilling process. The data may be collected while the well is drilling or shortly thereafter. Data typically collected and used by the geologist includes mud logs, well logs, and core. Mud logs: When drilling a well, fluid is used to cool the bit and carry rock fragments created by the drilling process away from the bit and to the surface. This fluid is called “mud”. Modern mud logs record the lithology of the drilled rocks based on the rock fragments and the presence of oil and gas carried to the surface by the mud. Well Logs : These are measurements of the rock properties inside the well bore. A few of the most common measurements used today include natural gamma radiation, resistivity, density, and neutron porosity. These measurements are made after the well has been drilled. Sophisticated tools are lowered to the bottom of the well. Rock property measurements are made as the tools are pulled out of the well. Core: These are samples of the rock taken either during drilling. Whole-diameter cores are taken by replacing the drill bit with a special coring tool. The tool allows cylinders of rock to be retrieved from the subsurface. Seismic data collected by the oil and gas industry uses sound waves to create an image of the subsurface, similar to how doctors use ultrasound to create images of a baby in a mother's womb. The process starts by sending vibrations through the earth. In the past, dynamite was used to generate vibrations and is still used in some places. Today, trucks that vibrate the ground are more common. The sound waves travel through the earth and are reflected from rock layers and other places where the rock properties change. Sensitive listening devices called geophones onshore record these reflections. The reflections are used to create images of the rocks in the subsurface. One important thing to know about seismic data is that it records the time it takes for the sound waves to travel down through the earth and reflect back to the geophone. These times must be converted to depth to generate maps, cross sections, and drilling prognosis. The data collected and used to analyze the field discussed here was extremely primate compared to modern data. At the time of discovery, all the data collected across the field, including well-log and seismic data, was based on analog technology. Geophysicists had to calculate by hand the time it took for each reflection to travel down and back and then convert that to depth. When this case went to trial in the 1980s, technology had advanced significantly since the time of discovery but it was still primitive compared to what we see today. Well logs were printed on folding paper a foot wide and tens of feet long. Interpretation was typically done by hanging the logs on walls or laying them out on drafting tables so the sand layers and formation boundaries could be correlated from well to well using colored pencils. [1] The purpose of this article is only to provide an example of some of the data types used by the oil and gas industry. The data types presented here have therefore been limited.
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