ASTM D5779-2008 317 Standard Test Method for Field Determination of Apparent Specific Gravity of Rock and Manmade Materials for Erosion Control《为冲刷控制现场测定岩石和人造材料的特殊外观重力的标准试验方法》.pdf
《ASTM D5779-2008 317 Standard Test Method for Field Determination of Apparent Specific Gravity of Rock and Manmade Materials for Erosion Control《为冲刷控制现场测定岩石和人造材料的特殊外观重力的标准试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D5779-2008 317 Standard Test Method for Field Determination of Apparent Specific Gravity of Rock and Manmade Materials for Erosion Control《为冲刷控制现场测定岩石和人造材料的特殊外观重力的标准试验方法》.pdf(3页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 5779 08Standard Test Method forField Determination of Apparent Specific Gravity of Rockand Manmade Materials for Erosion Control1This standard is issued under the fixed designation D 5779; the number immediately following the designation indicates the year oforiginal adoption or, in t
2、he case of revision, the year of last revision. A number in parentheses indicates the year of last reapproval. Asuperscript epsilon (e) indicates an editorial change since the last revision or reapproval.1. Scope*1.1 This test method covers the determination of the specificgravity of rock or man-mad
3、e materials for erosion control.1.2 This is a field test method to measure apparent specificgravity. For laboratory determination of bulk specific gravitysee Test Method D 6473.1.3 UnitsThe values stated in SI units are to be regardedas the standard. The inch-pound units in parentheses are givenfor
4、information only.1.4 All observed and calculated values shall conform to theguidelines for significant digits and rounding established inPractice D 6026.1.5 This standard does not purport to address all of thesafety concerns, if any, associated with its use. It is theresponsibility of the user of th
5、is standard to establish appro-priate safety and health practices and determine the applica-bility of regulatory limitations prior to use.2. Referenced Documents2.1 ASTM Standards:2C 670 Practice for Preparing Precision and Bias Statementsfor Test Methods for Construction MaterialsD 653 Terminology
6、Relating to Soil, Rock, and ContainedFluidsD 3740 Practice for Minimum Requirements for AgenciesEngaged in Testing and/or Inspection of Soil and Rock asUsed in Engineering Design and ConstructionD 4753 Guide for Evaluating, Selecting, and SpecifyingBalances and Standard Masses for Use in Soil, Rock,
7、 andConstruction Materials TestingD 4992 Practice for Evaluation of Rock to be Used forErosion ControlD 6026 Practice for Using Significant Digits in Geotechni-cal DataD 6473 Test Method For Specific Gravity And Absorptionof Rock For Erosion Control3. Terminology3.1 Definitions: For definitions spec
8、ific to this standard referto Terminology D 653.3.2 Definitions of Terms Specific to This Standard:3.2.1 field apparent specific gravitythe ratio of the massin air of a unit volume of impermeable rock or man-madematerial, to the mass of an equal volume of water. This issimilar to the definition of a
9、pparent specific gravity in Termi-nology D 653 except that non-distilled water is used for the testand the test can be run under a variety of temperatures.4. Summary of Test Method4.1 A specimen (block, chunk, slab, or piece) of rock ormanmade material is weighed in air and then weighed againwhile i
10、mmersed in water. Using the masses, the field specificgravity is calculated. The determined specific gravity can thenbe used to determine a mass per unit volume.5. Significance and Use5.1 Specific gravity is one factor used to determine therequired mass of individual particles used as gabion-fill, r
11、iprap,armor stone, breakwater stone, or other types of rock productsused for erosion control applications, and acceptibility of thesematerials for their intended use.NOTE 1The agency performing this test method can be evaluated inaccordance with Practice D 3740. Not withstanding statements on preci-
12、sion and bias contained in this test method: The precision of this testmethod is dependent on the competence of the personnel performing it andthe suitability of the equipment and facilities used. Agencies that meet thecriteria of Practice D 3740 are generally considered capable of competentand obje
13、ctive testing. Users of this test method are cautioned thatcompliance with D 3740 does not in itself ensure reliable testing. Reliabletesting depends on many factors; Practice D 3740 provides a means ofevaluating some of those factors.1This test method is under the jurisdiction ofASTM Committee D18
14、on Soil andRock and is the direct responsibility of Subcommittee D18.17 on Rock for ErosionControl.Current edition approved April 1, 2008. Published April 2008. Originallyapproved in 1995. Last previous edition approved in 2001 as D 5779 95a (2001).2For referenced ASTM standards, visit the ASTM webs
15、ite, www.astm.org, orcontact ASTM Customer Service at serviceastm.org. For Annual Book of ASTMStandards volume information, refer to the standards Document Summary page onthe ASTM website.1*A Summary of Changes section appears at the end of this standard.Copyright ASTM International, 100 Barr Harbor
16、 Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.6. Apparatus6.1 BalanceA balance or scale conforming to the require-ments of Specification D 4753 readable (with no estimation) to1 % or better of the mass of the test specimen and which hasprovisions for attaching to a specimen co
17、ntainer. For massesover 50 kg a load-cell, spring scale, or some other deviceaccurate to within 1 % of the mass may be used.6.2 Specimen ContainerA wire basket or sling or pan tobe attached to the scale and capable of holding the specimenand suspending it in water.6.3 Water bathA vessel filled with
18、a volume of waterlarge enough to submerge the specimen container withouttouching any of the vessels sides.6.4 An example apparatus is shown in Fig. 1.7. Sampling7.1 A source of rock to be sampled shall be guided byPractice D 4992. A source that is macroscopically uniform incolor, texture, mineralogy
19、, or some other visual property shallbe represented by a sample consisting of a minimum of fivespecimens of rock. A macroscopically nonuniform source shallbe represented by a minimum of eight samples of rock.7.2 Rock types that comprise less than 5 % of the totalsource, as determined from their macr
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