The Counters Blog

Porosity And Permeability Of Different Materials

Rocks are commonly divided into three major classes according to the processes that resulted in their formation. Since their constituent minerals are crystallized from molten material, igneous rocks are formed at high temperatures. Igneous rocks are subdivided into two categories: intrusive (emplaced in the crust), and extrusive (extruded onto the surface of the land or ocean bottom), in which case the cooling molten material is called lava. Most are deposited from the land surface to the bottoms of lakes, rivers, and oceans.

Porosity And Permeability | Duration 6 Minutes 27 Seconds

Layers may be distinguished by differences in colour, particle size, type of cement, or internal arrangement. The changes can be chemical (compositional) and physical (textural) in character. The recrystallization that takes place does so essentially in the solid state, rather than by complete remelting, and can be aided by ductile deformation and the presence of interstitial fluids such as water. Erosion includes weathering (the physical and chemical breakdown of minerals) and transportation to a site of deposition. The latter is the extent to which the bulk structure and composition are the same in all directions in the rock. On the other hand, the texture of gneiss is often described by its distinct banding.

Aphanitic is a descriptive term for small crystals, and phaneritic for larger ones. Most shales (the lithified version of clay) contain some silt. Blocks are fragments broken from solid rock, while bombs are molten when ejected. The volumetric portion of bulk rock that is not occupied by grains, crystals, or natural cementing material is termed porosity. Well-sorted indicates a grain size distribution that is fairly uniform. Total porosity encompasses all the void space, including those pores that are interconnected to the surface of the sample as well as those that are sealed off by natural cement or other obstructions. In a rock these general properties are determined by averaging the relative properties and sometimes orientations of the various grains or crystals. Knowledge of the distribution of underground rock densities can assist in interpreting subsurface geologic structure and rock type. Weight is the force that gravitation exerts on a body (and thus varies with location), whereas mass (a measure of the matter in a body) is a fundamental property and is constant regardless of location. Thus, density is often determined using weight rather than mass.

Basic Of Porosity And Permeability | Duration 8 Minutes 27 Seconds

Another property closely related to density is specific gravity. Figure 4, which illustrates the density distributions for granite, basalt, and sandstone. Basalt is, in most cases, an extrusive igneous rock that can exhibit a large variation in porosity (because entrained gases leave voids called vesicles), and thus some highly porous samples can have low densities.

The density of clastic sedimentary rocks increases as the rocks are progressively buried. It should be noted that the bulk density is less than the grain density of the constituent mineral (or mineral assemblage), depending on the porosity. For small stresses, the strain is elastic (recoverable when the stress is removed and linearly proportional to the applied stress). Bulk modulus (k ) is the ratio of the confining pressure to the fractional reduction of volume in response to the applied hydrostatic pressure. Bulk modulus is also termed the modulus of incompressibility. For elastic and isotropic materials, the elastic constants are interrelated. In the laboratory, one can simulate—either directly or by appropriate scaling of experimental parameters—several conditions.

Also, the role of fluids, particularly if they are chemically active, is investigated. The specimen is positioned on the baseplate; the pressure is applied by driving in pistons with a hydraulic press. Additional directed stress, as can be generated by large-scale crustal deformation (tectonism), can range up to 1 to 2 kilobars.

On a large scale, rock bodies exhibit physical and chemical variations and structural features. Figure 7 shows the generalized transition from brittle fracture through faulting to plastic-flow deformation in response to applied compressional stress and the progressive increase of confining pressure. Metamorphic rocks are those formed by changes in preexisting rocks under the influence of high temperature, pressure, and chemically active solutions. Metamorphism often produces apparent layering, or banding, because of the segregation of minerals into separate bands. Layered sandstone produces a gritty texture, whereas coquina may be rough with cemented shells occasionally producing a sharp edge. In contrast, obsidian tends to have a smooth glassy feel, whereas serpentine may feel platy or fibrous, and talc schist often feels greasy. That is to say, porosity is the ratio of void volume to the bulk volume (grains plus void space).

Depending on the type of close-packing of the grains, porosity can be substantial. A well-graded sediment is a (geologically) poorly sorted one, and a poorly graded sediment is a well-sorted one. It thus measures the pore volume that is effectively interconnected and accessible to the surface of the sample, which is important when considering the storage and movement of subsurface fluids such as petroleum, groundwater, or contaminated fluids. Since rocks are aggregates of mineral grains or crystals, their properties are determined in large part by the properties of their various constituent minerals. Some properties can vary considerably, depending on whether measured in situ (in place in the subsurface) or in the laboratory under simulated conditions.

Porosity And Permeability Lab | Duration 2 Minutes 12 Seconds

In strict usage, density is defined as the mass of a substance per unit volume; however, in common usage, it is taken to be the weight in air of a unit volume of a sample at a specific temperature.

Density should properly be reported in kilograms per cubic metre (kg/m3 ), but is still often given in grams per cubic centimetre (g/cm3 ). A useful way to assess the density of rocks is to make a histogram plot of the statistical range of a set of data. Figure 3 , (2) number of samples, and (3) standard deviation. A few fall well below the mode, even occasionally under 1 g/cm3.

Granite is an intrusive igneous rock with low porosity and a well-defined chemical (mineral) composition; its range of densities is narrow. Sandstone is a clastic sedimentary rock that can have a wide range of porosities depending on the degree of sorting, compaction, packing arrangement of grains, and cementation. This is because of the increase of overburden pressure, which causes compaction, and the progressive cementation with age. The pore-filling fluid is usually briny water, often indicative of the presence of seawater when the rock was being deposited or lithified. Saturated bulk density is higher than dry bulk density, owing to the added presence of pore-filling fluid. Shear modulus (μ) is the ratio of the applied stress to the distortion (rotation) of a plane originally perpendicular to the applied shear stress; it is also termed the modulus of rigidity. The volume strain is the change in volume of the sample divided by the original volume. Poisson’s ratio (σp ) is the ratio of lateral strain (perpendicular to an applied stress) to the longitudinal strain (parallel to applied stress). Two types of pressure may be simulated: confining (hydrostatic), due to burial under rock overburden, and internal (pore), due to pressure exerted by pore fluids contained in void space in the rock. An independent internal pore-fluid pressure also can be exerted.

This is approximately equal to the ultimate strength (before fracture) of solid crystalline rock at surface temperature and pressure (see below). In reality, on a microscopic scale there are grains and pores in sediments and a fabric of crystals in igneous and metamorphic rocks . Furthermore, conditions such as extended length of time, confining pressure, and subsurface fluids affect the rates of change of deformation.

Filter Press by

As the chambers fill, pressure inside the system will increase due to the formation of thick sludge. Major developments in filter press technology started in the middle of 20th century.

The presence of a centrifuge pump ensures the remaining suspended solids do not settle in the system, and its main function is to deliver the suspension into each of the separating chambers in the plate and frame filter.

Porosity And Permeability | Duration 6 Minutes 28 Seconds

The introduced slurry flows through a port in each individual frame, and the filter cakes are accumulated in each hollow frame. So when the separating chamber is full, the filtration process is stopped as the optimum pressure difference is reached.

Filter cake (suspended solid) accumulation occurs at the hollow plate frame, then being separated at the filter plates by pulling the plate and frame filter press apart.

A scraper can also be used, by moving from one chamber to another and scraping the cake off the cloth. The result is a high-speed filter press that allows increased production per unit area of filter. It is capable of holding 12 to 80 plates adjacent to each other, depending on the required capacity. The differences with the plate and frame filter are that the plates are joined together in such a way that the cake forms in the recess on each plate, meaning that the cake thickness is restricted to 32mm unless extra frames are used as spacers. This makes the membrane filter press a powerful and the most widely used system. This results in faster cycle and turnaround times, which lead to an increase in productivity. Other industrial uses for automatic membrane filter presses include municipal waste sludge dewatering,[15] ready mix concrete water recovery,[16] metal concentrate recovery, and large-scale fly ash pond dewatering. In filter press methodology, positive pressure filtration is used instead of vacuum filtration with high-energy consumption. Those are the most important factors that affect the rate of filtration. The filtration must be operated by increasing pressure difference to cope with the increase in flow resistance resulting from pore clogging.

Practically, maximum filtration rate is obtained when the filtration time is greater than the time taken to discharge the cake and reassemble the press to allow for cloth’s resistance. If extracting liquid phase is desired, then filter press is among the most appropriate methods to be used. It is possible to install moving blades in the filter press to reduce resistance to flow of liquid through the slurry. However, filter aids need to be able to remove from the filter cake either by physical or chemical treatment.

Describe The Concepts Of Porosity And Permeability | Duration 33 Minutes 11 Seconds

Thus the channels formed are constantly enlarged and therefore uneven cleaning is normally obtained. It flows through the whole thickness of the cakes in opposite direction first and then with the same direction as the filtrate. After washing, the cakes can be easily removed by supplying compressed air to remove the excess liquid. It is to prevent health risks to the local population and the workers that are dealing with the waste (filter cakes) as well as preventing negative impacts to our ecosystem. Another method is by incineration, which would destroy the organic pollutants and decrease the mass of the waste. In certain cases, it is crucial to compare characteristics and performances.

Therefore, the trend in increasing the pressure for the automatic filter press will keep on developing in the future. An alternative method has been introduced by using steam instead of air for cake dewatering.

In contrast to the conventional method, the system consists of membrane filter plates and heat exchanger plates, which are installed alternately in a filter press. The process uses the principle of pressure drive,[clarification needed ] as provided by a slurry pump. Optimal filling time will ensure the last chamber of the press is loaded before the mud in the first chamber begins to cake. However, there were many disadvantages associated with them, such as high labour requirement and discontinuous process. The device enables optimisation of the automatic filtration cycle, cake compression, cake discharge and filter-cloth washing leading to the increment in opportunities for various industrial applications. For each of the individual separating chambers, there is one hollow filter frame separated from two filter plates by filter cloths. As the filter cake becomes thicker, the filter resistance increases as well.

The filtrate that passes through filter cloth is collected through collection pipes and stored in the filter tank.

The cakes then fall off from those plates and are discharged to the final collection point. At the end of each run, the cloths are cleaned using wash liquid and are ready to start the next cycle. Its great disadvantage was the amount of labor involved in its operation. It consists of larger plate and frame filter presses with mechanical “plate shifters”.

What Is Porosity And Permeability? | Duration 3 Minutes 36 Seconds

It also contains a diaphragm compressor in the filter plates which aids in optimizing the operating condition by further drying the filter cakes. The option of the simultaneous filter plate opening system, for example, helps to realise a particularly fast cake release reducing the cycle time to a minimum. For this reason, these machines are used in applications with highly filterable products where high filtration speeds are required. The unmanned operating time of a fully automatic filter press is 24/7. Two plates join together to form a chamber to pressurize the slurry and squeeze the filtrate out through the filter cloth lining in the chamber. When the filter press is closed, a series of chambers is formed.

Compared to conventional filtration processes, it achieves the lowest residual moisture values in the filter cake. Membrane filter presses not only offer the advantage of an extremely high degree of dewatering; they also reduce the filtration cycle time by more than 50 percent on average, depending on the suspension. Many specialized applications are associated with different types of filter press that are currently used in various industries. However, a conventional filter press is a batch system and the process must be stopped to discharge the filter cake and reassemble the press, which is time consuming. Recessed plate press can form up to 32 mm of cake thickness.

Since then, there have been great enhancements in fabric quality and manufacturing technology that have made this issue obsolete. Moisture is typically 10-15% lower and less polymer is required—which saves on trucking and overall disposal cost. The improvement of the technology makes it possible to remove large amount of moisture at 16 bar of pressure and operate at 30 bars. If the concentration of solids in the feed tank increase until the solid particles are attached to each other. Coagulation as pre-treatment can improve the performance of filter press because it increases the porosity of the filter cake leading to faster filtration.

Moreover, if the filter cake is impermeable and difficult for the flow of filtrate, filter aid chemical can be added to the pre-treatment process to increase the porosity of the cake, reduce the cake resistance and obtain thicker cake. A better technique is by thorough washing in which the wash liquor is introduced through a different channel behind the filter cloth called washing plates. The wash liquor is normally discharged through the same channel as the filtrate. Therefore, before discharge waste stream into the environment, application of post-treatment would be an important disinfection stage. Since filter press would produce large amount of waste, if it was to be disposed by land reclamation, it is recommended to dispose to the areas that are drastically altered like mining areas where development and fixation of vegetation are not possible. It is usually done in a closed device by using a controlled flame. Efficiency improvements are possibl e in many applications where modern filter presses have the best characteristics for the job, however, despite the fact that many mechanical improvements have been made, filter presses still remain to operate on the same concept as when first invented. At the same time, many other types of filter could do the same or better job as press filters. A standard size filter press offers a filter area of 216 m2 , whereas a standard belt filter only offers approximately 15 m2. The conventional filter press mechanisms usually use mechanical compression and air to de-liquoring; however, the efficiency of producing low-moisture cake is limited.

Steam dewatering technique can be a competitive method since it offers product of low-moisture cake. Dewatering and drying of the resulting filter cake is thus done without a downstream drying process.

Filtration, washing and pressing out are carried out as usual. For thermal drying, hot steam and/or oil is applied to the working space behind the membrane and the filter cake is thermally dried accordingly.

Definition and Classification Of Fault Damage Zones: A Review and A New Methodological Approach by

Secondly, we propose an advanced field technique and data acquisition method to more accurately define a damage zone using the distribution of cumulative fracture frequency. The results show how this slope change can be a useful criterion in accurately defining the width of damage zones and some internal properties of fault zones. This will help us to gain a better understanding of fault damage zone properties and their scaling with fault displacement.

We believe that one of the fundamental reasons for this problem is strongly related to subjective definitions and inconsistent uses of the term ‘damage zone ’. We tested this method on new field and borehole observations as well as previously published data to identify damage zone boundaries, and express them as a change in slope gradients of the cumulative distribution of deformation structures.

We argue that this damage zone classification and definition method should be adopted and used to prevent discrepancies in field data.

Basaltic and Volcanic Rock Aquifers by

These igneous and metamorphic rocks are permeable only where they are fractured, and they generally yield only small amounts of water to wells. Although crystalline rocks are geologically complex, movement of water through the rocks is totally dependent on the presence of secondary openings; rock type has little or no effect on groundwater flow. The water moves from highland recharge areas to discharge areas, such as springs and streams at lower altitudes. Basaltic lavas tend to be fluid, and, they form thin flows that have considerable pore space at the tops and bottoms of the flows. Columnar joints that develop in the central parts of basalt flows create passages that allow water to move vertically through the basalt. In other places, local aquifers, such as those along stream valleys, might overlie the aquifers mapped. North of this line, glacial sand and gravel aquifers overlie bedrock aquifers in many places. Groundwater flow in the basaltic-rock aquifers is local to intermediate.

Unaltered pyroclastic rocks, for example, might have porosity and permeability similar to poorly sorted sediments. Silicic lavas tend to be extruded as thick, dense flows, and they have low permeability except where they are fractured. Numerous basalt flows commonly overlap, and the flows are separated by soil zones or alluvial material that form permeable zones. Basaltic rocks are the most productive aquifers in volcanic rocks. Permeability is greatest near the top and the bottom of the flow and least in the dense, center part of the flow. In some places, other, sometimes more productive, aquifers underlie those mapped. Local aquifers are not shown because of the scale of the map. Basaltic rocks form most of the volcanic-rock aquifers mapped. In most places, however, the thickness of these aquifers is 100 meters or less.

Porosity and Permeability by

The exploitation of natural resources, such as groundwater and petroleum, is partly dependent on the properties of porosity and permeability. Porosity represents the storage capacity of the geologic material. The more tightly packed the grains are, the lower the porosity.

The space surrounding each of the spherical marbles represents the void space. The primary porosity of unconsolidated sediments is determined by the shape of the grains and the range of grain sizes present. Primary porosity can range from less than one percent in crystalline rocks like granite to over 55% in some soils. Although a rock may be highly porous, if the voids are not interconnected, then fluids within the closed, isolated pores cannot move. In contrast, well-sorted sandstone closely replicates the example of a box of marbles cited above. Consequently, sandstones of this type have both high porosity and high permeability. The most conductive materials have permeability values that are millions of times greater than the least permeable. They are intrinsic characteristics of these geologic materials. Porosity is the ratio of the volume of openings (voids) to the total volume of material. The primary porosity of a sediment or rock consists of the spaces between the grains that make up that material.

Using a box of marbles as an example, the internal dimensions of the box would represent the volume of the sample. The porosity of the box of marbles would be determined by dividing the total void space by the total volume of the sample and expressed as a percentage. In poorly sorted sediments, those with a larger range of grain sizes, the finer grains tend to fill the spaces between the larger grains, resulting in lower porosity. The porosity of some rock is increased through fractures or solution of the material itself.

Permeability is a measure of the ease with which fluids will flow though a porous rock, sediment, or soil. The degree to which pores within the material are interconnected is known as effective porosity. The range of values for permeability in geologic materials is extremely large.

Sandstone by

Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to tectonic compression within orogenic belts.

The most common cementing materials are silica and calcium carbonate, which are often derived either from dissolution or from alteration of the sand after it was buried. This type of grain would be a main component of a lithic sandstone. Common accessory minerals include micas (muscovite and biotite), olivine, pyroxene, and corundum. One is to call the sandstone an arenite, and the other is to call it a wacke. Cement is a secondary mineral that forms after deposition and during burial of the sandstone. In sandstone where there is silica cement present, the quartz grains are attached to cement, which creates a rim around the quartz grain called overgrowth. Calcite cement is an assortment of smaller calcite crystals. Such components are quartz, feldspars,[8] and lithic fragments.

Even though sandstones have very simple compositions which are based on framework grains, geologists have not been able to agree on a specific, right way, to classify sandstones. Visual aids are diagrams that allow geologists to interpret different characteristics about a sandstone.

The stage of textural maturity chart illustrates the different stages that a sandstone goes through. This chart shows the difference between immature, submature, mature, and supermature sandstones. Folk’s dual textural and compositional maturity concepts into one classification system. Folk’s schemes is that it is better able to “portray the continuous nature of textural variation from mudstone to arenite and from stable to unstable grain composition”. These pure quartz sands result from extensive weathering that occurred before and during transport. These feldspar-rich sandstones come from rapidly eroding granitic and metamorphic terrains where chemical weathering is subordinate to physical weathering. Sandstone has been used for domestic construction and housewares since prehistoric times, and continues to be used.

It has also been used for artistic purposes to create ornamental fountains and statues. This makes sandstone a common building and paving material including in asphalt concrete. Because of the hardness of individual grains, uniformity of grain size and friability of their structure, some types of sandstone are excellent materials from which to make grindstones, for sharpening blades and other implements.

Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Sandstones are clastic in origin (as opposed to either organic , like chalk and coal, or chemical , like gypsum and jasper). Finally, once it has accumulated, the sand becomes sandstone when it is compacted by the pressure of overlying deposits and cemented by the precipitation of minerals within the pore spaces between sand grains. The different types of feldspar can be distinguished under a petrographic microscope. Lithic framework grains are pieces of ancient source rock that have yet to weather away to individual mineral grains, called lithic fragments or clasts. Quartz is the most common silicate mineral that acts as cement. The overgrowth retains the same crystallographic continuity of quartz framework grain that is being cemented. The cement adheres itself to the framework grains, this adhesion is what causes the framework grains to be adhered together. The porosity and permeability are directly influenced by the way the sand grains are packed together. For groundwater, work permeability may be measured in gallons per day through a one square foot cross section under a unit hydraulic gradient.

These minerals make up the framework components of the sandstones. Matrix may also be present in the interstitial spaces between the framework grains. When plotted correctly, this model of analysis creates for a meaningful quantitative classification of sandstones. A stage of textural maturity is a chart that shows the different stages of sandstones. As the sandstone becomes more mature, grains become more rounded, and there is less clay in the matrix of the rock. Quartz arenites are sandstones that contain more than 90% of siliceous grains. This weathering removed everything but quartz grains, the most stable mineral. Examples include volcanic and metamorphic clasts, though stable clasts such as chert are common in lithic are nites. Quartz wackes are uncommon because quartz arenites are texturally mature to supermature. Greywacke sandstones are a heterogeneous mixture of lithic fragments and angular grains of quartz and feldspar or grains surrounded by a fine-grained clay matrix.

Sandstone was a popular building material from ancient times.

It has been widely used around the world in constructing temples, homes, and other buildings. Some sandstones are resistant to weathering, yet are easy to work.

Which Of The Following Has Higher Permeability? Carbonates Sandstone Or Shale? by

There are very high permeability and very low permeability examples of both sands and carbonates. It is more easily defined as a seal or a cap for true reservoirs. How is the permeability of coral limestone measured?

What is the difference between shale oil and crude oil?

True shale, which does not include those horizons included in the current ‘shale’ revolution, has no effective permeability. At the other end of the spectrum, consider limestone or dolomite caves with house size or larger cavities with basically unlimited permeability.

So if you are looking for examples, the above offers some end points but to say a carbonate or a sandstone by definition has better porosity or permeability is not a confirmable possibility. What is the difference between oil shale, shale oil and shale gas?

Permeability Earth Sciences by

Permeabilities are more commonly in the range of tens to hundreds of millidarcies. Such “tight” rocks are usually artificially stimulated (fractured or acidized) to create permeability and yield a flow. Permeability values for sandstones range typically from a fraction of a darcy to several darcys. For a rock to be considered as an exploitable hydrocarbon reservoir without stimulation, its permeability must be greater than approximately 100 md (depending on the nature of the hydrocarbon – gas reservoirs with lower permeabilities are still exploitable because of the lower viscosity of gas with respect to oil). Unconsolidated sands may have permeabilities of over 5000 md. These terms refer to the quality that the permeability value in question is an intensive property of the medium, not a spatial average of a heterogeneous block of material[clarification needed ] [further explanation needed ] ; and that it is a function of the material structure only (and not of the fluid). Gas permeability of reservoir rock and source rock is important in petroleum engineering, when considering the optimal extraction of shale gas, tight gas, or coalbed methane.

The tensor is positive definite as the component of the flow parallel to the pressure drop is always in the same direction as the pressure drop. The permeability of a medium is related to the porosity, but also to the shapes of the pores in the medium and their level of connectedness. High permeability will allow fluids to move rapidly through rocks.

The concept of permeability is of importance in determining the flow characteristics of hydrocarbons in oil and gas reservoirs, and of groundwater in aquifers. This may also be called the intrinsic permeability or specific permeability. The permeability tensor is always diagonalizable (being both symmetric and positive definite).

Porosity by

Void fraction usually varies from location to location in the flow channel (depending on the two-phase flow pattern). The porosity of a rock, or sedimentary layer, is an important consideration when attempting to evaluate the potential volume of water or hydrocarbons it may contain. There is a clear proportionality between pore throat radii and hydraulic conductivity.

If the proportionality between pore throat radii and porosity exists then a proportionality between porosity and hydraulic conductivity may exist. For example: clays typically have very low hydraulic conductivity (due to their small pore throat radii) but also have very high porosities (due to the structured nature of clay minerals), which means clays can hold a large volume of water per volume of bulk material, but they do not release water rapidly and therefore have low hydraulic conductivity. Porosity is not controlled by grain size, as the volume of between-grain space is related only to the method of grain packing. Aggregation involves particulate adhesion and higher resistance to compaction.

Furthermore, it cannot help model the influence of environmental factors which affect pore geometry. The characterisation of pore space in soil is an associated concept. This can replace the primary porosity or coexist with it (see dual porosity below). This can create secondary porosity in rocks that otherwise would not be reservoirs for hydrocarbons due to their primary porosity being destroyed (for example due to depth of burial) or of a rock type not normally considered a reservoir (for example igneous intrusions or metasediments). Understanding the morphology of the porosity is thus very important for groundwater and petroleum flow. In fractured rock aquifers, the rock mass and fractures are often simulated as being two overlapping but distinct bodies.

While porosity is inherent in die casting manufacturing, its presence may lead to component failure where pressure integrity is a critical characteristic. Note that this method assumes that gas communicates between the pores and the surrounding volume. Strictly speaking, some tests measure the “accessible void”, the total amount of void space accessible from the surface (cf. The principal complication is that there is not a direct proportionality between porosity and hydraulic conductivity but rather an inferred proportionality. Also, there tends to be a proportionality between pore throat radii and pore volume. However, as grain size or sorting decreases the proportionality between pore throat radii and porosity begins to fail and therefore so does the proportionality between porosity and hydraulic conductivity.

Well sorted (grains of approximately all one size) materials have higher porosity than similarly sized poorly sorted materials (where smaller particles fill the gaps between larger particles). Connected porosity is more easily measured through the volume of gas or liquid that can flow into the rock, whereas fluids cannot access unconnected pores. Porosity is controlled by: rock type, pore distribution, cementation, diagenetic history and composition. Rocks normally decrease in porosity with age and depth of burial.

There are exceptions to this rule, usually because of the depth of burial and thermal history. This is due to soil aggregate formation in finer textured surface soils when subject to soil biological processes. This seems counterintuitive because clay soils are termed heavy , implying lower porosity. Porosity of subsurface soil is lower than in surface soil due to compaction by gravity. This can be a result of chemical leaching of minerals or the generation of a fracture system. Delayed yield, and leaky aquifer flow solutions are both mathematically similar solutions to that obtained for dual porosity; in all three cases water comes from two mathematically different reservoirs (whether or not they are physically different). Porosity may take on several forms from interconnected micro-porosity, folds, and inclusions to macro porosity visible on the part surface. Porosity may also lead to out-gassing during the painting process, leaching of plating acids and tool chatter in machining pressed metal components. In practice, this means that the pores must not be closed cavities.

Why Is Stone Porous? by

Igneous stones tend to have a low porosity, whereas metamorphic and sedimentary stones have higher porosity because of how they’re made up of tiny grains of material that, even though they’re compacted very tightly together, don’t fit together perfectly enough to not leave gaps. Pe rmeability is the ability of a material to transmit fluids. Therefore if a material is porous and permeable, it is more able to absorb liquids and other materials. Granite is relatively non-porous compared to other common countertop materials, though it still has some porosity. Marble is also fairly porous but not as much as limestone and sandstone. A big red mark is the last thing you want on your pure white marble slab!

Prevents the stone from being scratched and etched, though the sealant itself can be scratched and scraped.

Because stone is a natural material, there are some quirks that sometimes can’t be controlled. Sealing is non-negotiable, and thankfully it’s something that can be done quickly and easily at home.

This is because of the way stones are formed—whether it’s the slow compacting of tiny grains of organic matter or recrystallizing under intense heat and pressure, tiny gaps are left between the individual grains or crystals, which forms the pores.

Let’s investigate this issue further and find out how you can keep your stone looking brand new for years to come. Permeability is a related concept but isn’t the same thing as porosity. Fluids are transmitted by pores and the capillary structures they build within something—in this case, a stone. This can be a good thing for stone in some respects: the tiny pores are great at filtering water!

Limestone and sandstone are highly porous and readily absorb liquids, and are particularly prone to etching, and wearing away when they come into contact with acids. Staining is also a problem with more porous stones, especially darkly-colored liquids like red wine. Gives the stone a glossy appearance but can often darken the color. To test your stone’s porosity, put a few drops of water on the counter and wait a few seconds. If the water remains pooled on the surface, you’re good to go. Got a question about stone porosity and different sealants?

Porosity and Permeability Kit by

A wide product selection—from gel chambers to power supplies, centrifuges and pipets. We have the compound microscope you are looking for!

Exciting activities that make science active and fun!

Activities cover all disciplines and numerous subjects and topics. Porosity and permeability also can affect the extent that certain environmental issues, such as water pollution, impact different areas. After finding the volume of water each substrate can hold, students then compare the permeability of the different substrates and determine how each may affect the ability of water to move beneath the surface. Try a fresh approach with these interactive and engaging lessons. Hands-on experiments are a great way to help them understand the science behind the “magic”, especially for kinesthetic learners. Most are low or no cost and are varied enough to appeal to students with different learning styles.

In this activity, students examine 3 different substrates and determine the porosity of each.

What Are The Differences Between Porosity and Permeability? by

What are the differences between porosity and permeability?

What is physical meaning of permeability and what is the difference between high and low permeability?

What is the relation between void ratio and permeability?

What are the factors that affect membrane permeability?

How can you compare and contrast porosity and permeability?

In fabrics, what is the difference between air permeability and porosity?

How do porosity and permeability of the soil affect groundwater flow?

Can you distinguish between porosity and permeability? Permeability is an intrinsic property of a rock and is a measure of the ease with which a fluid is transmitted (via a pressure differential) through a rock. What are the characteristics between infiltration, hydraulic conductivity and permeability?

In materials science, what is the difference between diffusivity and permeability?

What is the difference between pore size and porosity of a material?

What is difference between permeability and seepage?

What is the difference between infiltration and permeability?


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