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# Determination of bulk density True density and porosity practical

Calculate the porosity of a soil sample that has a bulk density of 1.35 g/cm3. Assume the particle density is 2.65 g/cm3. Porosity = (1- (r b / r d) x 100 = (1- (1.35/2.65)) x 100 = 49% 7 Porosity can be calculated if bulk density and particle density are known. Bulk density is soil mass divided by unit volume. In its natural state, a soil's volume includes solids and pores, therefore, a sample must be taken without compaction or crumbling to correctly determine bulk density Shraddha Nalawade Physical pharmaceutics-II Experiment No.

### Practice problems: Porosity and bulk densit

• ed by the method specified in ISO 5018, the bulk density, apparent porosity and true porosity are deter
• Porosity (├Ė) = 100- bulk density/particle density*100% = 1-pb/pp) *100% Bulk density (Pb)=1.2g/cm3 Particle density will be 2.65g/cm3 Porosity (├Ė)=1-1.2/2.65) *100% = 55% The pore space of a soil is the space occupied by air and water
• 30/07/52 Density and porosity/S.T.Rattanachan 9 Apparent solid Volume = = the difference between dry weight ( D ) and the immersed weight ( I ) of piece. S -I = volume of open pores + sealed pores + solid S -D = Vol. open pores D -I = Vol. of sealed pore + solid Bulk density Weight = D App. Vol. S -I True density = Weight True Vol
• S.3.6. BULK DENSITY AND TAPPED DENSITY OF POWDERS BULK DENSITY The bulk density of a powder is the ratio of the mass of an untapped powder sample and its volume including the contribution of the interparticulate void volume. Hence, the bulk density depends on both the density of powder particles and the spatial arrangement of particles in th
• 2. If a soil has a high bulk density, what are the implications about porosity and aeration of the soil? 3. Given that a soil has a particle density of 2.64 g / cm3 and 50 % pore space, what is its bulk density? 4. The bulk density of a soil may be thought of as the mass of soil relative to th
• ing the density of foodstuffs, and summarizes the volumetric deter
• ation of bulk density and true porosity' issued by the International Organization for Standardization (ISO) was adopted by the Bureau of Indian Standards on the recommendation of the Refractories Sectional Committee and approval of the Metallurgical Engineering Division Council ### Bulk Density and Particle Density La

1. Density was nearly constant at 1.452 g/ml in all rice varieties; in paddy, the value was around 1.182 g/ml for round varieties and around 1.224 g/ml for others. Bulk density varied appreciably in both rice (0.777-0.847) and paddy (0.563-0.642 g/ml), and so did porosity (41-46% in rice, 46-54% in paddy)
2. A sample of calcium oxide powder with a true density of 3.203 and weighing 131.3 gm was found to have a bulk volume of 82cm3 when placed in a 100 ml graduated cylinder.calculate the porosity. The volume of the particle is (131.3g /3.203gcm-3) =41cm3 ĒĀĄĒ╝Ć = (vb- vp)/ vb = (82-41)/ 82 =0.5├Ś 100=50% 6
3. The formula for bulk density is (mass of dry soil) / (total volume of soil), 1 - (bulk density/particle density) for porosity, and (volume of pores) / (volume of solids) for void ratio
4. ation of the structural properties of a material is based on concerning structural properties data (true density, apparent density, and porosity) of various foodstuffs, versus time. (a) 2 4 9 16 18.
5. The bulk density of MR219 rice seed was measured at different moisture contents and found to increase at various levels; at 14.26% it was 517.70kg/m3 and a significant increase was observed when the moisture content increased to 22.50% with bulk density value of 543.544kg/m3. Simila 3.3 Bulk Density by measurement For uniform rectangular refractory shapes the simplest way of measuring Bulk Density is by dividing Dry Weight by Bulk Volume which is calculated from measured dimensions. This is the recommended procedure for measuring Bulk Density of insulation bricks (containing >40 % true porosity) (ISO 5016 and ASTM C134) Formation bulk density is a function of matrix density, porosity, and fluids contained in the pore space. Formation bulk density measured by the log must be corrected for borehole irregularities. Convert bulk density to porosity using charts in a log interpretation chartbook, or calculate porosity from bulk density using this equation porosity= (1-(bulk density/true density)*100 In the formula we have to use the bulk density or tapped density in numerator? I have used toluene displacement method to measure the true density The bulk density is influenced by the preparation, treatment and storage of the sample material. A method for measuring the bulk and tapped density of powders is described in the European Pharmacopoeia chapter 2.9.34. More about the methods. Bulk method 1: The bulk density is obtained by adding a known mass of powder to a graduated cylinder. Density and Porosity. The density of particles, powders, and compacts is an important property affecting the performance and function of many pharmaceutical materials. MPS uses five different state-of-the-art tools to measure density. By definition, all density measurements involve the measurement of mass and volume. Mass is determined with an analytical balance and the key to obtaining.

Calculate the bulk density and porosity of the sample, based on the formulas presented in the Background section.. PART TWO: Particle Density Particle density (as well as bulk density) of a sand can be easily approximated in the laboratory by the following procedure. 1. Weigh 50 g of dry sand and use a funnel to quantitatively transfe ŌÖ╗ MICROMERITICS ŌÖ╗ĒĀĮĒ▒©ŌĆŹĒĀĮĒ┤¼ A science and technology of small particles is called micromeriticsĒĀĮĒ▒ēĒĀ╝Ē┐╗ Dear Students Our PART-3 video lecture contain mainly about de.. In the case of parboiled paddy, bulk density and angle of repose increased from 507 to 564┬Ę8 kg/m 3 and 39┬Ę90 to 43┬Ę89┬░, respectively, with an increase in moisture content from 12┬Ę24 to 43┬Ę53% d.b. True density and porosity decreased from 1411 to 1342 kg/m 3 and from 64┬Ę08 to 57┬Ę91% respectively, with an increase in moisture content. 37. DRY-BULK DENSITY: ITS USE AND DETERMINATION1 Kathleen A. Dadey,2 Tom Janecek,3 and Adam Klaus4 ABSTRACT Sediment dry-bulk density values are essential components of mass accumulation rate calculations. This manuscript presents three equations to calculate dry-bulk density from laboratory measurements of physical properties that have been.

### Determination of bulk density, true density and porosity

• highest density at 2.78 g/cm3 and lowest porosity at 0.61%. Sample 5 had the lowest density at 0.67 g/cm3 and the highest porosity at 38.01%. This demonstrated the inversely proportional relationship of porosity and density. The helium porosity of two core samples were found to be 24.39% and 39.40%
• When eroded soil particles fill pore space, porosity is reduced and bulk density increases. Tillage and equipment travel in compacted soil layers results with increased bulk density, most notably a plow pan (Figures and 4). Tillage 3 prior to planting temporarily decreases bulk density on the surface but increases at the depth of tillage
• ation of the bulk density and true porosity of shaped insulating refractory products. 2 Normative references The following standards contain provisions which, through reference in this text, constitute provisions of this International Standard

### measuring bulk density, porosity and - SlideShar

The bulk density was determined by measuring the volume of a known mass of powder that had been passed through a screen into a volume-measuring device, and calculating the bulk density by dividing the mass by the volume. The average bulk density of the guaifenesin sample studied was found to be 0.39 g/mL The average porosity of the sample was 0.47. This was determined through the previously discussed equation using the calculate bulk density. These results for the first sample are as follows: f = 1 ŌłÆ (1.496 g cm 3 2.65 g cm 3) f = 0.435 These results indicate typical bulk density. Since bulk densities usually range from 1.0 to 2.0 g/cm 3 Determination of Bulk Density, True Density and Porosity: the average bulk density of the grains were determined using the standard test weight procedure reported by Singh and Goswami (1996) and Gupta and Das (1998) by filling a container of 500 ml with the seeds from a height of 150 mm at a constant rate and then weighing the content Hands on practical session. 4 8. Determination of bulk density, true density and porosity. At the end of the practical student should be able to demonstrate the concept of bulk density: To find out the bulk density, tapped density, angle of repose and other rheological properties of the powders. Hands on practical session. 4 9 the soil. You will compare the bulk density, particle density, and porosity of two soils varying widely in texture. You will also contribute data to the determination of a bulk density profile for a fine-textured soil. Exercise A. Measurement of Bulk Density Using a Soil Core 1. Your lab instructor will provide you with sand. 2 Whereas the Parliament of India has set out to provide a practical regime of right to Determination of porosity and density using saturation and buoyancy; and d) Determination of porosity and density using 2.2.8 Density or Bulk Density or Mass Density (p)LLLqMw kg/m3 2.2.9 Relative Density The total porosity content was determined by comparison of the bulk density to the true density of the material. Density measurements were obtained by determining their weight in water in conjunction with the Archimedes method. The true density was determined for porosity free samples in the same manner as porous samples The bulk density of a material is the ratio of the mass to the volume (including the interparticulate void volume) of an untapped powder sample. The tapped density is obtained by mechanically tapping a graduated cylinder containing the sample until little further volume change is observed

The purpose of the measurements was to gain sufficient information on grain density to permit application of the general information or pattern to the bulk water content determinations on the small syringe samples. Bulk density, porosity, and other properties could then be calculated without using volume measurements from the syringes The bulk density of a powder is the ratio of the mass of an untapped powder sample and its volume including the contribution of the interparticulate void volume. Hence, the bulk density depends on both the density of powder parti-cles and the spatial arrangement of particles in the powder bed. The bulk density is expressed in grams per mL (g/mL porosity tools). Density log: Porosity is calculated from the mass-balance relationship: where pb is the bulk density, 0 is the porosity, pma is the matrix density, and pf is the pore fluid density. If a sandstone, then the matrix density is 2.65 gm/cc (quartz), if a limestone, the matrix density is 2.71 gm/cc (calcite); if a dolomite Determination of bulk density, apparent porosity and true porosity BS EN 993-1:2018 Methods of test for dense shaped refractory products. BS 1902-6:1986 Methods of testing refractory materials Figure 4-1. Schematic presentation of soil water relationships. If a soil has a large porosity, the bulk density will be low because bulk density is the mass of dry soil per volume. If the soil volume increases and the mass stays constant, the bulk density goes down and porosity goes up. Therefore, bulk density can be used to estimate soil porosity

### True Density and Apparent Density During the Drying

SUGGESTED METHOD FOR POROSITY/DENSITY DETERMINATION USING SATURATION AND BUOYANCY TECHNIQUES 1. SCOPE (a) The test is intended to measure the porosity, the dry density and related properties of a rock sample in the form of lumps or aggregate of irregular geometry density of a substance by Eq. (13.1). The bulk density of a rock depends upon the solid minerals of which it is composed, its porosity, and the density of the fluids filling that porosity. Hence, the formation density tool is useful in the determination of porosity, the detection of low density fluid

This document specifies a method for the determination of the bulk density, apparent porosity and true porosity of dense shaped refractory products. NOTE For shaped insulating refractory products, the bulk density and true porosity are determined in accordance with EN 1094ŌĆæ4 IS 1528-12: Methods of Sampling and Physical Tests for Refractory Materials, Part 12: Method for Determination of Bulk Density and true porosity of shaped insulating refractory products by Bureau of Indian Standard Dense shaped refractory products ŌĆö Determination of bulk density, apparent porosity and true porosity This standard has been revised by ISO 5017:2013 General informatio

Where: Db = Bulk density (g/cm3) M = Mass of oven-dry soil (g) V = Volume of cylinder (cm3) Comparison of bulk density of different particles. Larger pores Smaller pores Generally bulk density of soil ranged Less porosity Greater porosity from 1.1 to 1.8 g/cm3. Bulk density of soil varies widely with soil texture and structure True Density The true or solid density defined as the ratio of a given mass of sample to its volume is determined by the water displacement method. Accordingly, a known weight (50g) of sample is poured into a 100cm3 fractionally graduated cylinder containing 50cm3 distilled water. The volume of water displaced by the seeds is observed. The true. Determination of bulk density, apparent porosity and true porosity Produits r├®fractaires fa├¦onn├®s denses ŌĆö D├®termination de la masse volumique apparente, de la porosit├® ouverte et de la porosit├® totale INTERNATIONAL STANDARD ISO 5017 Third edition 2013-01-15 Reference number ISO 5017:2013(E) This is a preview of ISO 5017:2013 surface area, porosity and thousand grains weight increased with increasing moisture content. On the other hand, bulk density, true density and sphericity were found to decrease with increase in moisture content. The prototype dehuller was designed and fabricated with a dehulling surface which can dehul moist grain without clogging. Th

### Some physical properties of paddy and rice and their

• ation of bulk density, apparent porosity and true porosity' issued by the International Organization for Standardization (ISO) was adopted by the Bureau of Indian Standards on the recommendation of the Refractories Sectional Committee and approval of the Metallurgical Engineering Division Council
• ed using water or another liquid which was expected to fill the pores i
• porous texture. This article describes the porosity, color, texture, and microscopic analysis of potatoes dried using MVD, heated air (HAD), and freeze drying (FD). The porosity was calculated from a ratio of apparent density and true density. A mathematical model for calculating true density from moisture content and apparent density was derived
• The relationship of bulk density and porosity is reciprocal. As one increases, the other decreases. Picture a brick. The brick is nearly 100% solid, so we'd say it has a high bulk density. Now picture a big sponge with lots of nooks and crannies of different sizes. The sponge is approximately 50% pore space, so we'd say it has a.
• ing formation chemical composition or lithology and allows a better porosity deter Bulk density (mass of dry soil/total soil volume): 395 g/300 cm 3 = 1.32 g/cm Particle Density: Mass of dry soil = 25.1 g Volume of dry soil = 9.5 mL (cm3) To calculate particle density (mass of dry soil/volume of particles only): 25.1 g/9.5 cm 3 = 2.64 g/cm Porosity: Using these values in the equation for porosity: 1 - x100% Bulk Density. 2.2.2 Determination of the bulk, true density and porosity The method of mass-volume relationship by Fraser et al.(1978) was adopted in determining the bulk density of the baobab fruit pulp powder. The sample was filled in a cylinder of predetermined volume and was gently tapped against a flat surface to get the new volume Elements of porosity determination._____ 2 Effect of bulk volume on porosity_____- 2 density. Apparent porosity, often called effective or net porosity, is a measure of the apparent void volume of a porous medium and is true bulk volume would be obtainable by dimensioning. Conside DIN EN 1094-4:1995 Insulating refractory products - Determination of bulk density and true porosity. The document specifies a method for determination of the bulk density and true porosity of shaped insulating refractory products

### Porosity - SlideShar

• ation of density ratio and porosity The density ratio D r is the ratio of true density to bulk density expressed as a percentage as follows: D r ┬╝ q t q b 100. ├░4├× Porosity (P) was computed (Jain & Bal, 1997)as P ┬╝ q t q b q t 100. ├░5├× Reported values of all density characteristics are means of 10 replications. 2.2
• Log Derived Porosity Crossplot Porosity ŌĆóDerived from the crossplot of neutron and density logs, using the appropriate matrix density. ŌĆóThe apparent total porosity thus obtained is then corrected for shale effects to derive the effective porosity. ŌĆóIn clean water bearing formations, the crossplot porosity (total porosity) is similar to that derived from the density log
• (ii) The bulk density must have been measured by methods that adequately account for void spaces (vugs, porosity, etc), moisture and differences between rock and alteration zones within the deposit. (iii) Direct assumptions for bulk density estimates used in the evaluation process of the different materials

- Density porosity is too high - Neutron porosity is too low - Neutron porosity < Density porosity - Cross-over - Be aware, cross-overs may also be caused by lithological differences as an affect of the scaling N D 2 D 2 N ND 3 2 3 1 2 Žå When a powder sample is analyzed using helium pycnometry (ASTM B923), the resulting True or Skeletal Density describes the density of the particles that make up the powder. Only non-porous materials are described by the term True Density, with Skeletal Density being applied to materials with any significant porosity This type of data can be used to determine different types of density: bulk density, apparent density and eventually true density if all the available porosity can be adequately accessed during the mercury porosimetry experiment

porosity) thereby correlates only to the total pore volume. Most of the reported literature on porosities used the gas pyc-nometer. The gas pycnometer also requires accurate mass mea-surements of pellets to evaluate the speci’¼üc weight (true density or solids density), while the true solids volume of pellets deter-mined under gas pressure The bulk density is an important in packaging requirement and is often 2-20% of true density Tapped Bulk Density : Tap bulk density is measured for powdery samples. The volume is measured after tapping the powdery material so that the product is adjusted to intergranular spaces, but it cannot eliminate all the intergranular spaces The borehole caliper and density correction curves are used to validate the quality of the bulk density readings. The foregoing discussion on sands provides an answer for porosity that is correct, but it reflects the average porosity over the depth of resolution of the tools (i.e., approximately 3 ft) Theoretical density: The ratio of the mass of a collection of discrete pieces of solid material to the sum of the volumes of said pieces, the solid material having an ideal regular arrangement at the atomic level (ASTM). X True density (also called True particle density); The mass of a particl

### What is the difference between bulk density, tapped

Title: POROSITY DETERMINATION 1 POROSITY DETERMINATION FROM LOGS Coring may not be practical in unconsolidated BULK DENSITY AND POROSITY Read: Chapter 1 (p. 12-17), and 6 (p. 93-105) Introduction to Environmental Soil Physics Soils are often described. Relative density, or specific gravity, is the ratio of the density (mass of a unit volume) of a substance to the density of a given reference material. Specific gravity for liquids is nearly always measured with respect to water at its densest (at 4 ┬░C or 39.2 ┬░F); for gases, the reference is air at room temperature (20 ┬░C or 68 ┬░F). The term relative density is often preferred in. V olumetric density measurements using pressure range from vacuum to 50 psi (345 kPa) and temperature range from sub ambient to 50C, with parallel relative humidity (RH) data (0-100%) RH analysis in the pressure and temperature range, sorption and kinetic data from multiple headspace extraction; Designed especially for true density measurements of fine powders and foam The volume change of helium in a constant volume chamber allows determination of solid volume. The ratio of sample mass to its true (sold) volume gives its true density. The volume of porosity open to the sample surfaces can also be measured, allowing determination of apparent (skeletal) density or analysis of open-cell foams

Porosity, ╬Ą (%) indicates the amount of pores in the bulk material and was calculated as per Mohsenin (1980). The porosity of the seed was calculated from the average values of bulk density and true density using the relationship. where, Žü b = bulk density (g/cm3); Žü t = true density (g/cm3) 2.6. Determination of frictional properties 2.6.1 The determination of volume is more challenging, usually due to samples having irregular shapes or being powders of varying degree. Additionally, it needs to be noted that volume, and thus density, may be defined differently if pores are included (raw density) or excluded (true / absolute density) into the solid samples volume This part of EN 993 specifies a method for the determination of the bulk density, apparent porosity and true porosity of dense shaped refractory products. Note: For shaped insulating refractory products, the bulk density and true porosity are determined in accordance with EN 1094-4 The true density was then calculated using equation below: 3 Weight of seed (g) True Density (g/cm ) Rise in tolune level (cm )3 = Determination of density ratio and porosity of seed: The density ratio (D r) is the ratio of true density to bulk density expressed as percentage as follows: ├▒ D 10 r ├▒ t b = ├Ś and was calculated as perDemir et.

### Density and Porosity: Literature Data Compilation for

This document specifies a method for the determination of the bulk density, apparent porosity and true porosity of dense shaped refractory products. NOTE For shaped insulating refractory products, the bulk density and true porosity are determined in accordance with EN 1094-4 Soils - Part 2: Physical Properties of Soil and Soil Water. Next Page. Soils - Part 2: Physical Properties of Soil and Soil Wate Porosity: The true measure of silage density Keith A. Bryan for Progressive Dairyman gas-filled porosity. Bulk density is 62.4 pounds per cubic foot, and dry matter density is 21.8 gas-filled porosity is closely related to as-fed density and allows for practical measurement on-farm. It is the true metric of silag 11. Soil texture has no impact on soil porosity. True False. 12. Soil porosity is not related to soil bulk density. True False. 13. An accepted value of soil particle density is 2.65 g/cm3. True False. 14. Aggregation of soil particles has a direct influence on bulk density True False. 15. It is difficult to alter a soil's bulk density. True.

### Density-neutron log porosity - AAPG Wik

For example, a soil having bulk density of 1.5 and particle density of 2.65. Calculate the porosity of the soil. % pore space = 100 (1-1.5/2.65 In the example Figures 1 and 2, the syringe was filled with corn silage (35 percent DM), and the resulting calculations provide the basis for discussing gas-filled porosity.. Thirty grams of corn silage was placed in the syringe, and the plunger was pushed to 60 cc. Bulk density (as-fed density) is 31.2 pounds per cubic foot, and DM density is 10.9 pounds per cubic foot - not very desirable. Determine the soil bulk density, the porosity, the volumetric water content and the; You have a 100 cm^3 container of a high clay soil that has a bulk density of 1.25 g\ cm^3. The average surface. ### How to measure the apparent porosity and bulk density of

4) From the weight and bulk volume of the powder calculate bulk density and bulkiness. 5) From bulk density value calculate the bulkiness of the powder sample. Procedure for determination of true density and porosity of a powder sample: 1) Find out the weight of a clean, dry, specific gravity bottle (SGB), let it be W1 Granule density and bulk density of the gran┬Ł ulations were varied . by . changing the concentrations of bis┬Ł muth aubcarbonate in the formula. All tablets were made at a fixed rate of tableting using standardized settings of the fill, pressure, and overload adjustments. The inter┬Ł relationship between granule density and bulk density wa Bulk density determined by solid displace┬Ł ment and true density determined by pycnometry yielded porosity measurements of 0.9 for bread and 0.6 for cooki es The introduction of the ISO 9000 quality standard resulted in renewed interest and pressure on industry to strengthen their quality and metrology standards. To meet this renewed interest Practical Density Measurement and Hydrometry provides invaluable, contemporary information on mass metrology. The book highlights the principles of physics involved and the technology needed to accurately. Bulk Density. Bulk density is a very important characteristic of substances such as powders, granules, and other particles like solid substances. Bulk density is defined as the mass of a bulk material divided by the volume occupied by that material. To understand this concept of bulk density, one must first understand what bulk materials are

### Bulk and Tapped Density Particle Analytica

bulk = bulk rock volume V dry = total dry weight of the rock r matrix = mean density of the matrix minerals. It should be noted that the porosity does not give any information concerning pore sizes, their This is also true for the other ordered packing lattices, but not true for the rando BULK DENSITY. b ma 1 f Matrix Measures electron density of a formation Strong function of formation bulk density Matrix bulk density varies with lithology Sandstone 2.65 g/cc Limestone 2.71 g/cc Dolomite 2.87 g/cc. Fluids in flushed zone POROSITY FROM DENSITY LOG Porosity equation. ma b. ma f. Fluid density equation. f mf Sxo h 1 Sx An accurate determination of bulk density starts with proper sampling. Acceptable procedures ensure that the collected sample represents the soil's natural condition and using a simplified tin can sampler, a liquid displacement technique, and a sampling device designed for use by soil scientists. Tin Can Sampling Metho The bulk density of soil depends greatly on the mineral make up of soil and the degree of compaction.The density of quartz is around 2.65 g/cm┬│ but the (dry) bulk density of a mineral soil is normally about half that density, between 1.0 and 1.6 g/cm┬│. In contrast, soils rich in soil organic carbon and some friable clays tend to have lower bulk densities (<1.0 g/cm┬│) due to a combination of. Calculate the bulk density (g/mL) by the formula m 0 /100 and record the average of 3 determinations using 3 different powder samples. 2. Tapped density The tapped density is an increased bulk density attained after mechanically tapping a container containing the powder sample. The tapped density is obtained by mechanically tapping Measuring density of solid, liquid and viscous samples on an analytical or precision balance - fast and easy process with Density Kit and balance application. We explain best procedures for density determination: buoyancy and displacement methods, both based on Archimedes' Principle. More ┬ Here, we propose a transformation based on determination of reservoir properties from acoustic and density properties. We have tried to determine the porosity and saturation logs from sonic velocity and density of three wells drilled during the First National Gas Hydrate Programme (NGHP- 01) LAB REPORT FOR PERMEABILITY AND POROSITY. Tolulope Afolabi. Related Papers. Petroleum Reservoir Rock and Fluid Properties s e c o n d e d i t i o n. By Isaias Herrera. Report about permeability. By Nizar Ali. Formation Evaluation MSc Course Notes. By Bhaskara Adjie. FUNDAMENTALS OF PETROLEUM RESERVOIR ENGINEERING In a Geological Survey report prepared for the U.S. Atomic Energy Commission, Manger (1963) summarized porosity and bulk density measurements for sedimentary rocks. He tabulated more than 900 items of porosity and bulk density data for sedimentary rocks with up to 2,109 porosity determinations per item

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