The OIP (Optical Image Profiler) is a direct push fluorescence detector tool used for the delineation of non-aqueous phase liquid (NAPL) hydrocarbon fuels and oils. The OIP-UV probe is designed with UV and visible light sources which are directed out a sapphire window. As the optical image probe is advanced into the subsurface, the UV light source will induce fluorescence of the fuel polycyclic aromatic hydrocarbons (PAHs). This fluorescence is captured by an onboard camera which operates at 30 images per second. Images are saved throughout the advancement of the log and still photos are taken using UV and visible light sources each rod addition as well as at operator chosen depths. Soil fluorescence images (20 per ft) are saved throughout the log and can be reviewed in Direct Image® Viewer after the log is complete. The OIP-G is available for heavier fuel or oil products.
= Tool String Diagram (TSD)
What is Geoprobe® Direct Image® OIP?
OIP is a logging tool that uses real time analysis of fluorescence images to map position and relative concentration of non-aqueous phase hydrocarbons. Images are saved (20 per foot) in the log for later review and confirmation.
The OIP-UV is a tool for mapping light non-aqueous phase liquids (LNAPL), residual LNAPL, and light oils. The OIP-UV system utilizes a 275nm ultraviolet (UV) light emitting diode (LED) to produce fluorescence from the polycyclic aromatic hydrocarbons (PAHs) contained in fuels and light oils. The UV light is directed out a sapphire window in the side of the probe (Figure 1) onto the soil. When LNAPL level fuels are present, the PAH molecules will absorb the UV light energy and shortly afterwards emit a light photon (fluorophore) which is the resultant fluorescence. Directly behind the sapphire window, the onboard camera captures images of the soil and any fluorescence produced by hydrocarbon contaminants present. The acquisition software analyzes each pixel of the images taken for the presence of color typical of fuel fluorescence. If there is no fuel present in the formation, or it is not in high enough concentration, then the returned camera image will appear black or dark under the UV light source. The OIP acquisition software logs percent area fluorescence with depth. The OIP-UV probe contains a visible as well as UV LEDs. The visible images are useful for determination of soil color, texture and occasionally confirming the presence of fuel or oil LNAPL globules.
The camera within the OIP probe operates at 30 frames per second with the log % area fluorescence (%AF) value being an average of all the images taken over a 0.05ft (1.5cm) interval. As the log is reviewed in Direct Image® Viewer, the user can click on the log and a green line will show up across the log which corresponds to a specific depth. The image saved from that depth will display if the OIP Image Display graph is shown. In Figure 2 the depth of the displayed saved image is 24.20ft, it is a UV image with the actual image being displayed in the "captured" image section. The "analyzed" image indicates which pixels within the image display fluorescent color consistent with the color expected for fuel fluorescence. There are two colors that may show up in the analyzed image: red which corresponds to the darker blue colors of the image and green which corresponds to areas of high brightness either due to very low color saturation or high brightness of the image. This is used in an attempt to isolate out possible false mineral fluorescence. The overlaid image takes both the captured image and analyzed image and overlays them so the operator can identify areas that are being counted as fluorescence. Images are saved as the probe is moving for every 0.05ft. The red dots on the right side column of the image display graph are depths that "Still Images" were taken. This will contain both UV and visible light still images on the OIP-UV probe. The OIP-G fluorescence detector probe takes images using a 520nm green laser diode and an infrared LED.
The OIP system software saves 20 images per foot (65 per meter), an example portion of the saved images that an OIP-UV log would contain is shown in Figure 3. These images are saved as the OIP-UV probe is advanced into the subsurface with a typical OIP log containing hundreds of images and being a few hundred mb in size depending upon terminal log depth and amount of color present in the images. Where there is no NAPL or residual NAPL present the images are black, where hydrocarbon NAPL is present blue fluorescence is seen within the images.
The OIHPT-UV Log in Figure 4 displays the following graphs (left to right) electrical conductivity, HPT injection pressure, OIP % image area fluorescence, depth specific saved UV images, depth specific saved visible images, and estimate of hydraulic conductivity (K). The red dots to the right of the saved images indicate locations of still UV and visible images saved in the file.
The OIP-G log in Figure 5 was performed on a creosote site in the northeast US. The OIP-G probe, which induces fluorescence utilizing a 520nm green laser diode (LD), returns a fluorescence image in the orange-red color range as depicted in the saved images from 10-20ft in the right column of the log. The red dots are the saved still images which are taken with the 520nm green LD and an infrared (IR) LED.
When the probe is stopped to add rods, still images will be captured with both available light sources in the OIP probe. Still images can be captured at any time an operator desires by stopping the probe advancement and selecting a button in the software. The process only takes a few seconds to complete and probe advancement can resume. These still images provide greater image clarity and an opportunity to look at the soil and fuel under visible light. Visible images provide the investigator an opportunity to observe soil color and texture in-situ. Occasionally when hydrocarbon NAPL is present in a saturated sand formation NAPL globules are evident in both the UV and visible images (Figure 6).
DI Viewer is a free program downloadable from the link below which allows the user to display any of the Direct Image® log types (MIP, OIP, HPT, EC). With this program the user can display the raw data .zip files of each saved graph of an individual log in single log view or compare them to other logs using the overlay and cross sectional view functions. Log specific QA data is also accessible with this software which also allows one to print or export the logs data for 3D modeling or into .jpg or .png files.
The OIP software does not automatically provide any distinct product designation based upon the fluorescence image returned from the oil. Each fuel or oil type may give a slightly different coloration of the respondent fluorescent image. Assuming that the coloration of the QA diesel and motor oil images are consistent throughout the project, if the coloration of the fuel fluorescence has changes in the borehole or between logs then the different is likely due to either different levels of weathering of the same fuel/oil product or there are two separate fuel/oils present.
No concentration can not be determined. OIP Fluorescence only occurs when fuel or oil NAPL or residual NAPL is present. The higher the % fluorescence response the greater the distribution of fuel NAPL.
The standard OIP-UV fluorescence graph is the result of a software filter that analyzes all of the pixels within an OIP-UV image that is displaying coloration (Hue, Saturation and Value) that is consistent with common fuels and oils. The resulting fluorescence is the % of the pixels within the image that are displaying this general fluorescence coloration (% of the image area). This is related more to distribution of fuel NAPL – the higher the % Fluorescence and the thicker the zone of fluorescence the more product NAPL that is present.
Yes, there can be false positive fluorescence such as calcium carbonates found in calcite mineral deposits or seashells. These calcium carbonates can be a bigger issue with false positives on the 520nm Green light source. Paper and clothing can also provide false positive fluorescence readings but may be less likely to occur in a natural setting. To help aid in determining if the fluorescence is real or a false positive, we strongly encourage numerous visible images being captured during advancement through fluorescing zones to compare the UV or G fluorescence image to the grains in the visible/IR image.
The OIP-G probe has a 520nm green light source, which as the name states is in the visible light range displayed as a green light. Because of this we are not able to use a visible light as the secondary source. We would see a significant amount of residual green light in the visible image. Also because of this in our green probe we must add a filter over the camera to block all the light wavelengths that will cause background coloration from reflected source light from the soil. With that filter in place over the camera we lose all natural color of the soil so using an infrared source results in a black and white color image. We do not worry about the color of the soil but can still get an indication of the texture of the soil which can still aid in interpretation of the log fluorescence or if false positives are present.
Absolutely. If there is great interest in soil color and texture, or work trying to amp a specific coloration within the geologic formation such as dark peat or in inject carbon zone these can stand out under the visible light source. The probe can be advanced using the visible light as the primary light source.
BTEX components fluoresce in the UV range and jet fuel/kerosene fluorescence can be challenging with the 275nm UV light source. If the fuel that is gasoline with the primary contaminants being BTEX or jet fuel it is possible that little fluoresce will be observed in the UV logs and images while a sheen could be observed in an adjacent soil or groundwater sample.
No chlorinated DNAPL solvents will not fluoresce on their own without help from something else. Many chlorinated solvents like Trichloroethylene and Trichloroethane have been used as degreaser in industrial manufacturers. In this case there is a likelihood that the comingled oils and greases within the DNAPL will fluorescence under the OIP-UV excitation. We recommend a sample being collected and tested prior to mobilization for this purpose. Also, MIP can be used the track the chlorinated solvent plume from DNAPL to sub ppm levels.
Features & Options
What is Geoprobe® Direct Image® OIP?
OIP is a logging tool that uses real time analysis of fluorescence images to map position and relative concentration of non-aqueous phase hydrocarbons. Images are saved (20 per foot) in the log for later review and confirmation.
The OIP-UV is a tool for mapping light non-aqueous phase liquids (LNAPL), residual LNAPL, and light oils. The OIP-UV system utilizes a 275nm ultraviolet (UV) light emitting diode (LED) to produce fluorescence from the polycyclic aromatic hydrocarbons (PAHs) contained in fuels and light oils. The UV light is directed out a sapphire window in the side of the probe (Figure 1) onto the soil. When LNAPL level fuels are present, the PAH molecules will absorb the UV light energy and shortly afterwards emit a light photon (fluorophore) which is the resultant fluorescence. Directly behind the sapphire window, the onboard camera captures images of the soil and any fluorescence produced by hydrocarbon contaminants present. The acquisition software analyzes each pixel of the images taken for the presence of color typical of fuel fluorescence. If there is no fuel present in the formation, or it is not in high enough concentration, then the returned camera image will appear black or dark under the UV light source. The OIP acquisition software logs percent area fluorescence with depth. The OIP-UV probe contains a visible as well as UV LEDs. The visible images are useful for determination of soil color, texture and occasionally confirming the presence of fuel or oil LNAPL globules.
The camera within the OIP probe operates at 30 frames per second with the log % area fluorescence (%AF) value being an average of all the images taken over a 0.05ft (1.5cm) interval. As the log is reviewed in Direct Image® Viewer, the user can click on the log and a green line will show up across the log which corresponds to a specific depth. The image saved from that depth will display if the OIP Image Display graph is shown. In Figure 2 the depth of the displayed saved image is 24.20ft, it is a UV image with the actual image being displayed in the "captured" image section. The "analyzed" image indicates which pixels within the image display fluorescent color consistent with the color expected for fuel fluorescence. There are two colors that may show up in the analyzed image: red which corresponds to the darker blue colors of the image and green which corresponds to areas of high brightness either due to very low color saturation or high brightness of the image. This is used in an attempt to isolate out possible false mineral fluorescence. The overlaid image takes both the captured image and analyzed image and overlays them so the operator can identify areas that are being counted as fluorescence. Images are saved as the probe is moving for every 0.05ft. The red dots on the right side column of the image display graph are depths that "Still Images" were taken. This will contain both UV and visible light still images on the OIP-UV probe. The OIP-G fluorescence detector probe takes images using a 520nm green laser diode and an infrared LED.
The OIP system software saves 20 images per foot (65 per meter), an example portion of the saved images that an OIP-UV log would contain is shown in Figure 3. These images are saved as the OIP-UV probe is advanced into the subsurface with a typical OIP log containing hundreds of images and being a few hundred mb in size depending upon terminal log depth and amount of color present in the images. Where there is no NAPL or residual NAPL present the images are black, where hydrocarbon NAPL is present blue fluorescence is seen within the images.
The OIHPT-UV Log in Figure 4 displays the following graphs (left to right) electrical conductivity, HPT injection pressure, OIP % image area fluorescence, depth specific saved UV images, depth specific saved visible images, and estimate of hydraulic conductivity (K). The red dots to the right of the saved images indicate locations of still UV and visible images saved in the file.
The OIP-G log in Figure 5 was performed on a creosote site in the northeast US. The OIP-G probe, which induces fluorescence utilizing a 520nm green laser diode (LD), returns a fluorescence image in the orange-red color range as depicted in the saved images from 10-20ft in the right column of the log. The red dots are the saved still images which are taken with the 520nm green LD and an infrared (IR) LED.
When the probe is stopped to add rods, still images will be captured with both available light sources in the OIP probe. Still images can be captured at any time an operator desires by stopping the probe advancement and selecting a button in the software. The process only takes a few seconds to complete and probe advancement can resume. These still images provide greater image clarity and an opportunity to look at the soil and fuel under visible light. Visible images provide the investigator an opportunity to observe soil color and texture in-situ. Occasionally when hydrocarbon NAPL is present in a saturated sand formation NAPL globules are evident in both the UV and visible images (Figure 6).
DI Viewer is a free program downloadable from the link below which allows the user to display any of the Direct Image® log types (MIP, OIP, HPT, EC). With this program the user can display the raw data .zip files of each saved graph of an individual log in single log view or compare them to other logs using the overlay and cross sectional view functions. Log specific QA data is also accessible with this software which also allows one to print or export the logs data for 3D modeling or into .jpg or .png files.
The OIP software does not automatically provide any distinct product designation based upon the fluorescence image returned from the oil. Each fuel or oil type may give a slightly different coloration of the respondent fluorescent image. Assuming that the coloration of the QA diesel and motor oil images are consistent throughout the project, if the coloration of the fuel fluorescence has changes in the borehole or between logs then the different is likely due to either different levels of weathering of the same fuel/oil product or there are two separate fuel/oils present.
No concentration can not be determined. OIP Fluorescence only occurs when fuel or oil NAPL or residual NAPL is present. The higher the % fluorescence response the greater the distribution of fuel NAPL.
The standard OIP-UV fluorescence graph is the result of a software filter that analyzes all of the pixels within an OIP-UV image that is displaying coloration (Hue, Saturation and Value) that is consistent with common fuels and oils. The resulting fluorescence is the % of the pixels within the image that are displaying this general fluorescence coloration (% of the image area). This is related more to distribution of fuel NAPL – the higher the % Fluorescence and the thicker the zone of fluorescence the more product NAPL that is present.
Yes, there can be false positive fluorescence such as calcium carbonates found in calcite mineral deposits or seashells. These calcium carbonates can be a bigger issue with false positives on the 520nm Green light source. Paper and clothing can also provide false positive fluorescence readings but may be less likely to occur in a natural setting. To help aid in determining if the fluorescence is real or a false positive, we strongly encourage numerous visible images being captured during advancement through fluorescing zones to compare the UV or G fluorescence image to the grains in the visible/IR image.
The OIP-G probe has a 520nm green light source, which as the name states is in the visible light range displayed as a green light. Because of this we are not able to use a visible light as the secondary source. We would see a significant amount of residual green light in the visible image. Also because of this in our green probe we must add a filter over the camera to block all the light wavelengths that will cause background coloration from reflected source light from the soil. With that filter in place over the camera we lose all natural color of the soil so using an infrared source results in a black and white color image. We do not worry about the color of the soil but can still get an indication of the texture of the soil which can still aid in interpretation of the log fluorescence or if false positives are present.
Absolutely. If there is great interest in soil color and texture, or work trying to amp a specific coloration within the geologic formation such as dark peat or in inject carbon zone these can stand out under the visible light source. The probe can be advanced using the visible light as the primary light source.
BTEX components fluoresce in the UV range and jet fuel/kerosene fluorescence can be challenging with the 275nm UV light source. If the fuel that is gasoline with the primary contaminants being BTEX or jet fuel it is possible that little fluoresce will be observed in the UV logs and images while a sheen could be observed in an adjacent soil or groundwater sample.
No chlorinated DNAPL solvents will not fluoresce on their own without help from something else. Many chlorinated solvents like Trichloroethylene and Trichloroethane have been used as degreaser in industrial manufacturers. In this case there is a likelihood that the comingled oils and greases within the DNAPL will fluorescence under the OIP-UV excitation. We recommend a sample being collected and tested prior to mobilization for this purpose. Also, MIP can be used the track the chlorinated solvent plume from DNAPL to sub ppm levels.
Having the combo tool of OIP and HPT, we can find leaching pathways, not just for contaminated petroleum areas, but also for metals or something like that. We can hammer complex sites where there might be a lot of historical uses that led to a variety of contamination, and we can address it in one mobilization, reducing costs for the client up front, but also delivering this really comprehensive product at the back end.
- Loran Brooks, Engineer, Water & Environmental Technologies, Montana
Geoprobe Systems® manufactures all of the equipment needed for OIHPT logging. This equipment can be divided into two basic categories: surface instrumentation (OIP interface, data acquisition, and HPT controller), and downhole probes (including probes, trunklines, connectors, etc.).
A basic set of OIHPT instruments is shown in Figure 7 and includes the following:
Basic downhole OIP equipment is shown in Figure 8. There are many variations and combinations of this tooling, depending on the contaminant type, depth requirement and the lithology or permeability sensors that are to be used in combination with the OIP. The standard, most commonly deployed components are shown below:
Having HPT data along with the OIP-EC data provides the site investigator a powerful combination of logging tools. This tool provides the ability to simultaneously estimate soil permeability with the HPT, detect NAPL fluorescence with the OIP, and measure soil/pore fluid conductance with standard EC. The OIHPT probe and system can be operated with all sensors collecting data or it can be used to collect just HPT-EC data or just OIP-EC data depending upon project and weather considerations.
OIHPT-G probe utilizes a 520nm green laser diode to induce fluorescence on larger PAH contaminants such as Creosote, Coal Tars, Heavy Crude Oils and Bunker Fuels.
This OIHPT-CPT sub allows an operator to collect HPT injection pressure, OIP fuel fluorescence, and EC lithology along with CPT tip resistance, sleeve friction and U2 pore pressure when combined with the Nova cone. The tool can be operated without the NOVA cone by running with the thread solid point or with the NOVA cone by substituting the solid point with the NOVA cone. The OIHPT CPT sub is available in either ultraviolet-visible or green-infrared light source models depending upon the target contaminant requirements.
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Click on a section below to view information.
OIP-UVR provides added confidence when detecting lighter-end jet fuels.
ID: 14028 | Date:
Investing in OIHPT optical imaging system distinguishes services from other in region while providing clients a cost effective characterization.
ID: 12401 | Date:
Finkler Ambiental uses their Geoprobe® 6712DT in conjunction with Direct Image® MiHPT and OIP systems at a project site that serves as a storage plant for various fuels with more than 300 monitoring wells.
ID: 5774 | Date:
The Optical Imaging Profiler (OIP) is a new direct push photo-logging system developed by Geoprobe® that uses a down hole light source...
ID: 5245 | Date:
The Optical Image Profiler (OIP) is a direct push probe that uses UV fluorescence to...
ID: 5248 | Date:
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Engineering and building industry-leading drilling rigs, tooling, and techniques for the technical driller based on your needs to work safer and more efficiently.
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What is Geoprobe® Direct Image® OIP?
OIP is a logging tool that uses real time analysis of fluorescence images to map position and relative concentration of non-aqueous phase hydrocarbons. Images are saved (20 per foot) in the log for later review and confirmation.
The OIP-UV is a tool for mapping light non-aqueous phase liquids (LNAPL), residual LNAPL, and light oils. The OIP-UV system utilizes a 275nm ultraviolet (UV) light emitting diode (LED) to produce fluorescence from the polycyclic aromatic hydrocarbons (PAHs) contained in fuels and light oils. The UV light is directed out a sapphire window in the side of the probe (Figure 1) onto the soil. When LNAPL level fuels are present, the PAH molecules will absorb the UV light energy and shortly afterwards emit a light photon (fluorophore) which is the resultant fluorescence. Directly behind the sapphire window, the onboard camera captures images of the soil and any fluorescence produced by hydrocarbon contaminants present. The acquisition software analyzes each pixel of the images taken for the presence of color typical of fuel fluorescence. If there is no fuel present in the formation, or it is not in high enough concentration, then the returned camera image will appear black or dark under the UV light source. The OIP acquisition software logs percent area fluorescence with depth. The OIP-UV probe contains a visible as well as UV LEDs. The visible images are useful for determination of soil color, texture and occasionally confirming the presence of fuel or oil LNAPL globules.
The camera within the OIP probe operates at 30 frames per second with the log % area fluorescence (%AF) value being an average of all the images taken over a 0.05ft (1.5cm) interval. As the log is reviewed in Direct Image® Viewer, the user can click on the log and a green line will show up across the log which corresponds to a specific depth. The image saved from that depth will display if the OIP Image Display graph is shown. In Figure 2 the depth of the displayed saved image is 24.20ft, it is a UV image with the actual image being displayed in the "captured" image section. The "analyzed" image indicates which pixels within the image display fluorescent color consistent with the color expected for fuel fluorescence. There are two colors that may show up in the analyzed image: red which corresponds to the darker blue colors of the image and green which corresponds to areas of high brightness either due to very low color saturation or high brightness of the image. This is used in an attempt to isolate out possible false mineral fluorescence. The overlaid image takes both the captured image and analyzed image and overlays them so the operator can identify areas that are being counted as fluorescence. Images are saved as the probe is moving for every 0.05ft. The red dots on the right side column of the image display graph are depths that "Still Images" were taken. This will contain both UV and visible light still images on the OIP-UV probe. The OIP-G fluorescence detector probe takes images using a 520nm green laser diode and an infrared LED.
The OIP system software saves 20 images per foot (65 per meter), an example portion of the saved images that an OIP-UV log would contain is shown in Figure 3. These images are saved as the OIP-UV probe is advanced into the subsurface with a typical OIP log containing hundreds of images and being a few hundred mb in size depending upon terminal log depth and amount of color present in the images. Where there is no NAPL or residual NAPL present the images are black, where hydrocarbon NAPL is present blue fluorescence is seen within the images.
The OIHPT-UV Log in Figure 4 displays the following graphs (left to right) electrical conductivity, HPT injection pressure, OIP % image area fluorescence, depth specific saved UV images, depth specific saved visible images, and estimate of hydraulic conductivity (K). The red dots to the right of the saved images indicate locations of still UV and visible images saved in the file.
The OIP-G log in Figure 5 was performed on a creosote site in the northeast US. The OIP-G probe, which induces fluorescence utilizing a 520nm green laser diode (LD), returns a fluorescence image in the orange-red color range as depicted in the saved images from 10-20ft in the right column of the log. The red dots are the saved still images which are taken with the 520nm green LD and an infrared (IR) LED.
When the probe is stopped to add rods, still images will be captured with both available light sources in the OIP probe. Still images can be captured at any time an operator desires by stopping the probe advancement and selecting a button in the software. The process only takes a few seconds to complete and probe advancement can resume. These still images provide greater image clarity and an opportunity to look at the soil and fuel under visible light. Visible images provide the investigator an opportunity to observe soil color and texture in-situ. Occasionally when hydrocarbon NAPL is present in a saturated sand formation NAPL globules are evident in both the UV and visible images (Figure 6).
DI Viewer is a free program downloadable from the link below which allows the user to display any of the Direct Image® log types (MIP, OIP, HPT, EC). With this program the user can display the raw data .zip files of each saved graph of an individual log in single log view or compare them to other logs using the overlay and cross sectional view functions. Log specific QA data is also accessible with this software which also allows one to print or export the logs data for 3D modeling or into .jpg or .png files.