Porosity is the quality of being porous, or full of tiny holes. Liquids go right through things that have porosity. It is shown as a fraction of the volume of voids over the total volume, which is between 0 and 1, or between 0% and 100% as a percentage. Primary and secondary porosity can be read directly from neutron, density, and sonic logs.
The objective of this test is to determine the bulk volume,
grain volume, pore volume and effective porosity of
interconnected pores of a core sample with the use of liquid
saturation method.
1-To calculate plastic viscosity of the mud .
2-To calculate yield point.
Viscometer or rheometer is a device used to measure the viscosity and yield point of mud, A sample of mud is placed in a slurry cup and rotation of a sleeve in the mud.
Viscosity and yield point exp. by jarjis
Experiment Number 5: Yield Point.
Koya University.
Faculty of Engineering.
Drilling Lab
Supervised By Muhammad Jamal
Determine Plastic Viscosity, Apparent Viscosity, And Yield point of a drilling fluid (mud) by using Fann VG viscometer.
=============
This a report about Filtration. written by Jarjis Muhammad, Petroleum Engineering Dep. Koya University. For more Information please contact me: www.facebook.com/Jarjis.shaqlawaee
Rheology model 900 viscometer Mud Engineering Exp.Jarjis Mohammed
Rheology model 900 viscometer by jarjis
Experiment Number 7: Rheological Properties using Model 900 Viscometer.
Koya University.
Faculty of Engineering.
Drilling Lab
Supervised By Muhammad Jamal
=============
This a report about Rheological Properties using Model 900 Viscometer.. written by Jarjis Muhammad, Petroleum Engineering Dep. Koya University. For more Information please contact me: www.facebook.com/Jarjis.shaqlawaee
The objective of this test is to determine the bulk volume,
grain volume, pore volume and effective porosity of
interconnected pores of a core sample with the use of liquid
saturation method.
1-To calculate plastic viscosity of the mud .
2-To calculate yield point.
Viscometer or rheometer is a device used to measure the viscosity and yield point of mud, A sample of mud is placed in a slurry cup and rotation of a sleeve in the mud.
Viscosity and yield point exp. by jarjis
Experiment Number 5: Yield Point.
Koya University.
Faculty of Engineering.
Drilling Lab
Supervised By Muhammad Jamal
Determine Plastic Viscosity, Apparent Viscosity, And Yield point of a drilling fluid (mud) by using Fann VG viscometer.
=============
This a report about Filtration. written by Jarjis Muhammad, Petroleum Engineering Dep. Koya University. For more Information please contact me: www.facebook.com/Jarjis.shaqlawaee
Rheology model 900 viscometer Mud Engineering Exp.Jarjis Mohammed
Rheology model 900 viscometer by jarjis
Experiment Number 7: Rheological Properties using Model 900 Viscometer.
Koya University.
Faculty of Engineering.
Drilling Lab
Supervised By Muhammad Jamal
=============
This a report about Rheological Properties using Model 900 Viscometer.. written by Jarjis Muhammad, Petroleum Engineering Dep. Koya University. For more Information please contact me: www.facebook.com/Jarjis.shaqlawaee
Total (absolute) Porosity and Isolated Porosity MeasurementRaboon Redar
Absolute porosity is the percentage or volume of void spaces or porosity of rocks that can contain hydrocarbons. Porosity is the measure of a rock’s ability to hold hydrocarbons like oil and gas, water, and condensates. Absolute porosity contains effective (interconnected) and ineffective (isolated) porosity. Effective porosity is the volume of connected pores, but isolate is the pore volume which is not connected to the pore network. Isolated porosity can be significant in volcanic rocks and some carbonates.
This experiment will explain a procedure to get drilling mud with a range of density that requires for maintaining the borehole pressure as drilling goes dipper, the objective is generating a drilling mud; then it requires to rise the density by 0.1ppg and getting a drilling mud that is more dens.
Total (absolute) Porosity and Isolated Porosity MeasurementRaboon Redar
Absolute porosity is the percentage or volume of void spaces or porosity of rocks that can contain hydrocarbons. Porosity is the measure of a rock’s ability to hold hydrocarbons like oil and gas, water, and condensates. Absolute porosity contains effective (interconnected) and ineffective (isolated) porosity. Effective porosity is the volume of connected pores, but isolate is the pore volume which is not connected to the pore network. Isolated porosity can be significant in volcanic rocks and some carbonates.
This experiment will explain a procedure to get drilling mud with a range of density that requires for maintaining the borehole pressure as drilling goes dipper, the objective is generating a drilling mud; then it requires to rise the density by 0.1ppg and getting a drilling mud that is more dens.
Determining an unknown Density of a RockRaboon Redar
The main aim of this experiment is to find out the density of a rock using two basic ways. Density is defined as the mass of a substance per unit volume, and is highly variable in crustal rocks. Rock density is a physical characteristic that is governed by the chemical composition and pore spaces of a specific rock or rock type. Rock densities are useful to engineers, of course. They're also essential for geophysicists who must model the rocks of the Earth's crust for calculations of local gravity. In most cases, denser objects are also heavier.
index properties of soil, Those properties of soil which are used in the identification and classification of soil are known as INDEX PROPERTIES
Water content
Specific gravity
In-situ density
Particle size
Consistency
Relative Density
The reservoir (rock porosity and permeability)salahudintanoli
Reservoir rock is the one of the important component in petroleum system i.e without it petroleum system is impossible. This presentation contain all necessary information regarding reservoir rock.
Study on Physical and Mechanical Properties of Dispersive Soilijtsrd
This paper deals with determination of physical and mechanical properties of dispersive soil. Soil is the foundation material which supports loads from the overlaying structure. Soil dispersivity is mainly due to the presence of exchangeable sodium present in the structure. Dispersive soils are identified by an unstable structure, easily flocculated in water, and very erodible. Using dispersive clay soils in hydraulic structures, embankment dams, or other structures such as roadway embankments can cause serious engineering problems if these soils are not identified and used appropriately. Some important parameters of dispersive soil obtained from laboratory testing are investigated in this paper. Soil sample is taken from Mandalay at about 3ft depth. To determine physical properties of soil, water content determination, specific gravity test, grain size analysis, Atterberg limits test, crumb test. Standard Proctor compaction test, Unconfined Compression Strength UCS test are carried out to determine mechanical properties of soil. According to Unified Soil Classification System, the studied soil is in CH group and group name is lean clay with sand. From crumb test, sample has grade 4. Therefore, the studied soil is highly dispersive. Soe Soe War | Nyein Nyein Thant "Study on Physical and Mechanical Properties of Dispersive Soil" Published in International Journal of Trend in Scientific Research and Development (ijtsrd), ISSN: 2456-6470, Volume-3 | Issue-5 , August 2019, URL: https://www.ijtsrd.com/papers/ijtsrd26627.pdfPaper URL: https://www.ijtsrd.com/engineering/civil-engineering/26627/study-on-physical-and-mechanical-properties-of-dispersive-soil/soe-soe-war
Experimental Approach for Assessment of Liquefaction in Fine Sand and Silty Sandinventionjournals
The investigation is focused on the comparative study of the silty sand and fine sand soil in respect of the fine contents regarding liquefaction characteristics. The strategy is planned to obtain the locally available silty and fine sand in sufficient quantities. Thereafter these two were sieved to segregate the sand portion and fine contents so as to prepare the reconstituted samples of known percentage of fines in silty sand group and clean sand group, besides, these soil samples were again put to sieve analysis to estimate the grading of individual soil samples and specimen samples are prepared. The results of specimen samples suggested that as the percentage of fines increases then chance of liquefaction decreases.
Electricity and Electromagnetism (experimental study)Raboon Redar
You’ll understand the way to calculate and measure resistance in parallel and series circuits by knowing two of the three values of voltage, current, or resistance. In this experiment, there are 3 resistors, 1 power supply and wires you need for connecting resistors to each other, then to power supply. You can measure each resistor by an ohmmeter, voltages by voltmeter and currents by amperemeter (ammeter), while all of them can be measured by a multimeter. Use a multimeter for measuring resistance for better accuracy.
Physical Properties of different types of Metamorphic Rocks (Geology)Raboon Redar
Metamorphic rocks are rocks that have been modified by heat, pressure, and chemical processes, usually while buried deep below Earth's surface. Change to these extreme conditions changes the mineralogy, texture, and chemical composition of the rocks.
A rock is lustrous and shiny if it has Dolomite Crystall which is lustrous in front of the sun. Formation are some kinds of rocks which can be seperated due to some general principles like age, lithology and fossils, and when you separate them, you give them a name like: Sargalu, Surdash, Nawkalakan, Berserin, Bexma...etc
Physical Properties of different types of Sedimentary Rocks (Geology)Raboon Redar
The rock type, texture, grain size, composition, and other comments on the sedimentary rocks is shown...
Sediment is a material that is occurred naturally and broken down by processes of physical or chemical weathering, and erosion. Physical weathering like: Frost wedging, Unloading, Thermal Expansion and Biological activity. Chemical weathering like: Dissolution, Hydrolysis and Oxidation.
Weathering rates are a function of the rock type, slope (topography), structure, and the prevailing climate. Rocks that are most resistant are composed of minerals that are relatively unaffected by chemical weathering like: Quartz (that are more resistant than any other rock types). Sediments are transported by the action of wind, ice (glaciers), the gravity force acting on particles and most of them by water. Sediments can be classified based on their composition and grain size which is a good indicator of the energy or force required to move a grain of a given size.
Physical Properties of different types of Igneous Rocks (Geology)Raboon Redar
the texture, color, mineral composition, intrusive or extrusive, equivalent, felsic or mafic of the igneous rocks are discussed... (from the Greek word for fire) form from when hot, molten rock crystallizes and solidifies. The melt originates deep within the Earth near active plate boundaries or hot spots, then rises toward the surface. Igneous rocks are divided into two groups, intrusive or extrusive, depending upon where the molten rock solidifies.
Physical Properties of different types of Minerals (Geology)Raboon Redar
This report shows the luster, hardness, color, cleavage, streak, fracture, crystal system, chemical composition, and remarks of different types of minerals...
Geologists define mineral as any naturally occurring inorganic solid that has an orderly crystalline structure and can be represented by a chemical formula. A compound needs to exhibit these 5 characteristics to be called a mineral: naturally occurring, has to be solid substance, orderly crystallized structure, generally inorganic (not contain carbon), and should be represented by a chemical formula.
Chemical and Physical Properties of Earth's Layers and the Tectonic Plates (G...Raboon Redar
To determine the chemical composition inside the Earth indirect measurements are used. One way to determine composition is to measure how the density of rock changes with depth below the Earth’s surface. We can do this by measuring the speeds, because they move more quickly through dense rocks than through less dense rocks. From such measurements we know that density increases with depth, but not evenly. Knowing these different densities, we can estimate what the composition of the different layers must be. The layers of different chemical composition outward from the centre of the Earth are as follows: core, mantle, and crust.
Properties of different types of Rocks (Geology)Raboon Redar
This file shows the luster, hardness, color, cleavage, streak, fracture, crystal system, chemical composition, and remarks of different types of minerals... the texture, color, mineral composition, intrusive or extrusive, equivalent, felsic or mafic of the igneous rocks... and the rock type, texture, grain size, composition, and other comments on the sedimentary rocks... all in pictures and tables.
Dead – Weight piston gauge & Center of PressureRaboon Redar
The calibration of the Bourdon gauge is the aim of the dead weight pressure gauge experiment, while the center of pressure is the other test’s aim to find the resultant force (F) and center of pressure (hp). For testing and changing pressure gages, the death-weight pressures gage is used. The pressure is exerted by weights which are supported by weight. The latter has a piston that operates on hydraulic oil in the pipe system to show those pressures by a pressure gage that is also attached to the system. A Bourdon gage with a clear dial is included in the device. Thus, there is a simple identification of the display mechanism and the different adaptation choices.
The aim of the fluid flow rate experiment is to measure the fluid flow rate using a device called the hydraulic bench unit, which is also used to prove the Bernoulli’s Theorem Demonstration by measuring the overall pressure of the fluid flow.
The aim of this experiment is to standardize 0.1N Sodium Hydroxide (NaOH) which is an unstandard substance, by using standardized Hydrochloric acid (Na2CO3).
Liquid–liquid extraction (LLE) also known as solvent extraction is a method to separate compounds based on their relative solubility in two different immiscible liquids, usually water and an organic solvent. Liquid–liquid extraction is a separation process which is based on the different distribution of the components to be separated between two liquid phases.
Applications of Differential Equations in Petroleum EngineeringRaboon Redar
In modern science and engineering, differential equations are very important. Nearly all known physics and chemistry laws are indeed differential equations. Engineers, in order to investigate systems behavior, it is virtually necessary that they are able to model and solve physical problems with mathematical equations.
Geophysical methods in Hydrocarbon ExplorationRaboon Redar
Geophysical studies of the earth's interior include measurements on or near to the earth's surface that are dependent upon the physical properties of the internal distribution. Examination of these measurements can show how vertically and laterally the physical properties of the Earth's interior differ. Through operating on different scales, geophysical techniques can be used to investigate the localized upper crust area for engineering or other purposes.
Hierarchical Digital Twin of a Naval Power SystemKerry Sado
A hierarchical digital twin of a Naval DC power system has been developed and experimentally verified. Similar to other state-of-the-art digital twins, this technology creates a digital replica of the physical system executed in real-time or faster, which can modify hardware controls. However, its advantage stems from distributing computational efforts by utilizing a hierarchical structure composed of lower-level digital twin blocks and a higher-level system digital twin. Each digital twin block is associated with a physical subsystem of the hardware and communicates with a singular system digital twin, which creates a system-level response. By extracting information from each level of the hierarchy, power system controls of the hardware were reconfigured autonomously. This hierarchical digital twin development offers several advantages over other digital twins, particularly in the field of naval power systems. The hierarchical structure allows for greater computational efficiency and scalability while the ability to autonomously reconfigure hardware controls offers increased flexibility and responsiveness. The hierarchical decomposition and models utilized were well aligned with the physical twin, as indicated by the maximum deviations between the developed digital twin hierarchy and the hardware.
About
Indigenized remote control interface card suitable for MAFI system CCR equipment. Compatible for IDM8000 CCR. Backplane mounted serial and TCP/Ethernet communication module for CCR remote access. IDM 8000 CCR remote control on serial and TCP protocol.
• Remote control: Parallel or serial interface.
• Compatible with MAFI CCR system.
• Compatible with IDM8000 CCR.
• Compatible with Backplane mount serial communication.
• Compatible with commercial and Defence aviation CCR system.
• Remote control system for accessing CCR and allied system over serial or TCP.
• Indigenized local Support/presence in India.
• Easy in configuration using DIP switches.
Technical Specifications
Indigenized remote control interface card suitable for MAFI system CCR equipment. Compatible for IDM8000 CCR. Backplane mounted serial and TCP/Ethernet communication module for CCR remote access. IDM 8000 CCR remote control on serial and TCP protocol.
Key Features
Indigenized remote control interface card suitable for MAFI system CCR equipment. Compatible for IDM8000 CCR. Backplane mounted serial and TCP/Ethernet communication module for CCR remote access. IDM 8000 CCR remote control on serial and TCP protocol.
• Remote control: Parallel or serial interface
• Compatible with MAFI CCR system
• Copatiable with IDM8000 CCR
• Compatible with Backplane mount serial communication.
• Compatible with commercial and Defence aviation CCR system.
• Remote control system for accessing CCR and allied system over serial or TCP.
• Indigenized local Support/presence in India.
Application
• Remote control: Parallel or serial interface.
• Compatible with MAFI CCR system.
• Compatible with IDM8000 CCR.
• Compatible with Backplane mount serial communication.
• Compatible with commercial and Defence aviation CCR system.
• Remote control system for accessing CCR and allied system over serial or TCP.
• Indigenized local Support/presence in India.
• Easy in configuration using DIP switches.
Welcome to WIPAC Monthly the magazine brought to you by the LinkedIn Group Water Industry Process Automation & Control.
In this month's edition, along with this month's industry news to celebrate the 13 years since the group was created we have articles including
A case study of the used of Advanced Process Control at the Wastewater Treatment works at Lleida in Spain
A look back on an article on smart wastewater networks in order to see how the industry has measured up in the interim around the adoption of Digital Transformation in the Water Industry.
Saudi Arabia stands as a titan in the global energy landscape, renowned for its abundant oil and gas resources. It's the largest exporter of petroleum and holds some of the world's most significant reserves. Let's delve into the top 10 oil and gas projects shaping Saudi Arabia's energy future in 2024.
1. Soran University
Faculty of Engineering
Department of Petroleum Engineering
Petroleum Geology
Title: Porosity Measurement
Lab Number: 2
Name: Raboon Redar Muhammed
Lab Date: 13/10/2019
Supervisor(s): Mr. Foad Yousefi
Ms. Meriam
2. 1 | P o r o s i t y M e a s u r e m e n t
1. Aim
The main aim of this experiment is to find out the porosity of a rock.
2. Introduction
Porosity is the quality of being porous, or full of tiny holes. Liquids go right through things that have
porosity. (Vocabulary.com, 2019) It is shown as a fraction of the volume of voids over the total volume,
which is between 0 and 1, or between 0% and 100% as a percentage. Primary and secondary porosity can be
read directly from neutron, density, and sonic logs. (En.wikipedia.org, 2019) These tools do not measure
pore volume directly, rather they measure physical parameters of the formation and relate them to porosity
mathematically or empirically. (day,R,L and marsh,B,K, 1988). Below, the effective porosity is being
calculated which refers to the fraction of the total volume in which fluid flow is effectively taking place and
includes catenary and dead-end pores but excludes closed pores. This is very important for groundwater and
petroleum flow, as well as for solute transport.
3. Materials
1- Graduated cylinder
2- Water
3- Electric Balance
4- Slime
5- Bunsen burner
6- Beaker
7- Igneous Rock
4. Procedure
1. Measure the mass of the rock.
2. Measure the mass of one slime.
3. Use 2 or 3 slimes to cover the rock completely.
4. Measure the mass of the slime that was used to cover the rock completely.
5. Measure the volume of one slime, pour water into graduated cylinder, then put the slime into the
cylinder and measure the displaced water, displaced water is equal to the volume of the slime.
6. Find the density of the slime by the rule (ρ=mass of one slime / volume of one slime)
7. Use the density of the slime to find the volume of the covered slime that used to cover the rock by
knowing its mass and density (volume of all slime = mass of all slime / density of slime)
8. Put the rock covered with slime into a beaker filled with water, and measure the displaced water
which is equal to the volume of the rock covered with slime.
3. 2 | P o r o s i t y M e a s u r e m e n t
9. Subtract the slime volume from the rock covered with slime volume to get the bulk volume (rock
volume) by the rule (V bulk = V of rock covered with slime – V of slime).
10. Take out the rock’s slime, and use Bunsen burner to clear the rock from slime.
11. Put the rock into another beaker filled with water and measure the displacement water that is the
volume of the grains and the isolated pores.
12. Find porosity by that rule (φ = (Vbulk – Vgrain )/ Vbulk )
5. Calculations
Mass of the rock = 17.75g
Mass of the one slime = 9.1798g
Mass of the rock covered by slime = 55.05g
Mass of the covered slime used to cover the rock = mass of rock with slime - mass of the rock →
55.05g – 17.75g = 37.3g
Volume of one slime = displaced water = 7 cm3
Density of the slime = ρ = mass of one slime / volume of one slime = 9.1798/7 = 1.3114 g/cm3
Volume of the covered slime = mass of the covered slime / density of the slime →
37.3/1.3114 = 28.442 cm3
Volume of the rock covered with slime = displaced water = 31.55 cm3
Bulk volume = V of the rock covered with slime – V of slime = 31.55 – 28.442 = 3.108 cm3
Grain volume = displaced water = 2.5 cm3
Φ = (Vbulk – Vgrain)/ Vbulk = (3.108 – 2.5) / 3.108 = 0.19 × 100 = %19
6. Results
Rock Coated Rock One Slime Coated Slime Porosity Φ
Mass 17.75g 55.05g 9.1798g 37.3g
%19
Volume 2.5cm3 28.442cm3 7cm3 28.442cm3
Density 1.3114g/cm3 1.3114g/cm3
Table 1: Results of the experiment in a table.
4. 3 | P o r o s i t y M e a s u r e m e n t
7. Discussion
Be careful, putting the rock into a water without coating and measuring the displacement doesn't give the
volume of the bulk or the grains.
8. Conclusion
Pumic rocks usually have a porosity range between 64-85%, but human and random errors may have
occurred such as the inability to take accurate reading on the beaker. It can be said that the porosity of pumic
rock is always big because of its lithology, But that does not mean a reservoir with pumic rock is a good
reservoir, because factors such as fluid conductivity or permeability also effect too much.
9. References
Vocabulary.com. (2019). porosity - Dictionary Definition. [online] Available at:
https://www.vocabulary.com/dictionary/porosity [Accessed 19 Oct. 2019].
En.wikipedia.org. (2019). Porosity. [online] Available at: https://en.wikipedia.org/wiki/Porosity [Accessed
19 Oct. 2019].
Day, R.L. and Marsh, B.K., 1988. Measurement of porosity in blended cement pastes. Cement and Concrete
Research, 18(1), pp.63-73.