ASTM D4544-1986(2008) Standard Practice for Estimating Peat Deposit Thickness《泥炭沉积厚度的评估的标准实施规程》.pdf
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1、Designation: D 4544 86 (Reapproved 2008)Standard Practice forEstimating Peat Deposit Thickness1This standard is issued under the fixed designation D 4544; the number immediately following the designation indicates the year oforiginal adoption or, in the case of revision, the year of last revision. A
2、 number in parentheses indicates the year of last reapproval. Asuperscript epsilon (e) indicates an editorial change since the last revision or reapproval.1. Scope1.1 This practice uses a technique of probing to estimate thethickness of surficial peat deposits overlying mineral soil orbedrock. These
3、 estimates may be needed for energy, horticul-tural, or geotechnical purposes.1.2 This standard does not purport to address all of thesafety concerns, if any, associated with its use. It is theresponsibility of the user of this standard to establish appro-priate safety and health practices and deter
4、mine the applica-bility of regulatory limitations prior to use.1.3 This practice offers a set of instructions for performingone or more specific operations. This document cannot replaceeducation or experience and should be used in conjunctionwith professional judgment. Not all aspects of this practi
5、ce maybe applicable in all circumstances. This ASTM standard is notintended to represent or replace the standard of care by whichthe adequacy of a given professional service must be judged,nor should this document be applied without consideration ofa projects many unique aspects. The word “Standard”
6、 in thetitle of this document means only that the document has beenapproved through the ASTM consensus process.2. Referenced Documents2.1 NRC Canada Document:2Peat Testing Manual3. Terminology3.1 Definitions of Terms Specific to This Standard:3.1.1 peata naturally occurring organic substance derived
7、primarily from plant materials.4. Summary of Practice4.1 The resistance to penetration of a pushed or driven rodwill increase sharply at the boundary of a peat layer withunderlying mineral soil or bedrock. When this abrupt change ismeasured in a series of probings with an appropriate spacing,the thi
8、ckness and areal extent of peat can be defined and thevolume of peat may be calculated.4.2 Sampling of the peat may be required to determine thepeat characteristics.5. Significance and Use5.1 This practice allows the determination of the depth atwhich the resistance to penetration of a pushed or dri
9、ven rodincreases sharply. When the overlying material is peat and theunderlying one is mineral soil or bedrock, the depth of changemay be interpreted as the thickness of peat. Successive arealdeterminations of this depth, in combination with surfacemeasurements of the lateral extent of peat will all
10、ow calcula-tion of the volume of peat in the deposit.6. Interferences6.1 Sampling of the zone of contact of peat with underlyingmaterial is usually necessary to verify the interpretations ofmaterial change from the rod penetration resistances.6.2 Where the peat mineral transition zone is of signifi-
11、cant thickness, or where the peat is underlain by soft clays ormarls, further sampling and testing will be required (see 7.2).6.3 The frequency of sampling is highly dependent upon thephysical details of the deposit.6.4 Penetration of the rod may be prevented by wood piecesin the peat deposit. Data
12、should be examined and rechecked ifthis occurrence is suspected.6.5 The thin and flexible nature of the rod strings will limitthe depths of penetrating and sampling.7. Apparatus7.1 Graduated Steel RodsPenetration is achieved withgraduated steel rods of 9.5 6 1.0-mm diameter and 1.0 or1.2-m length,3w
13、hich can be threaded together to penetrate arange of thickness. The rods are ringed at 200-mm intervals foreasy estimation of depth. A ring with a short threaded end isscrewed into the last section and another rod or stick insertedhorizontally to facilitate pulling out the rod.1This practice is unde
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