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1、BRITISH STANDARD BS ISO 17313:2004 Soil quality Determination of hydraulic conductivity of saturated porous materials using a flexible wall permeameter ICS 13.080.40 ? Licensed Copy: sheffieldun sheffieldun, na, Sun Nov 26 03:29:48 GMT+00:00 2006, Uncontrolled Copy, (c) BSI BS ISO 17313:2004 This Br
2、itish Standard was published under the authority of the Standards Policy and Strategy Committee on 19 July 2004 BSI 19 July 2004 ISBN 0 580 44102 4 National foreword This British Standard reproduces verbatim ISO 17313:2004 and implements it as the UK national standard. The UK participation in its pr
3、eparation was entrusted to Technical Committee EH/4, Soil quality, which has the responsibility to: A list of organizations represented on this committee can be obtained on request to its secretary. Cross-references The British Standards which implement international publications referred to in this
4、 document may be found in the BSI Catalogue under the section entitled “International Standards Correspondence Index”, or by using the “Search” facility of the BSI Electronic Catalogue or of British Standards Online. This publication does not purport to include all the necessary provisions of a cont
5、ract. Users are responsible for its correct application. Compliance with a British Standard does not of itself confer immunity from legal obligations. aid enquirers to understand the text; present to the responsible international/European committee any enquiries on the interpretation, or proposals f
6、or change, and keep the UK interests informed; monitor related international and European developments and promulgate them in the UK. Summary of pages This document comprises a front cover, an inside front cover, the ISO title page, pages ii to v, a blank page, pages 1 to 13 and a back cover. The BS
7、I copyright notice displayed in this document indicates when the document was last issued. Amendments issued since publication Amd. No. DateComments Licensed Copy: sheffieldun sheffieldun, na, Sun Nov 26 03:29:48 GMT+00:00 2006, Uncontrolled Copy, (c) BSI Reference number ISO 17313:2004(E) OSI 4002
8、INTERNATIONAL STANDARD ISO 17313 First edition 2004-07-01 Soil quality Determination of hydraulic conductivity of saturated porous materials using a flexible wall permeameter Qualit du sol Dtermination de la conductivit hydraulique de matriaux poreux saturs laide dun permamtre paroi flexible BS ISO
9、17313:2004 Licensed Copy: sheffieldun sheffieldun, na, Sun Nov 26 03:29:48 GMT+00:00 2006, Uncontrolled Copy, (c) BSI IS:31371 O4002(E) DPlcsid Fremia ihTs PDF file may ctnoian emdebt dedyfepcaes. In ccaocnadrw eith Aebods licensilop gnic,y this file mairp eb ynted iv roweb detu slahl ton ide ebtlnu
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12、. In tlnu ehikletneve y ttah lborp aem leratign to it is f,dnuo lpsaee inform ttneC ehlar Secrteiraat ta the serddaig sleb nevwo. ISO 4002 Athgir lls serevr.de selnUs towrehise specfidei, trap on fo thsi ilbupctanoi may cudorper ebtu ro dezilina ni dey fomr yb ro nam y,snae lecetrinoc ro mecinahcal,
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14、ro Pulbisdehi n Switlrez dna ii ISO 4002 Allr ithgsr esedevr BS ISO 17313:2004 Licensed Copy: sheffieldun sheffieldun, na, Sun Nov 26 03:29:48 GMT+00:00 2006, Uncontrolled Copy, (c) BSI IS:31371 O4002(E) I SO 4002 All irthgs ersedevr iii Contents Page Forewordiv Introduction v 1 Scope 1 2 Terms and
15、definitions. 1 3 Significance and use 1 4 Reagents 2 5 Apparatus 2 6 Test specimen . 5 6.1 Specimen dimensions 5 6.2 Undisturbed specimen . 5 6.3 Laboratory-compacted specimen . 5 6.4 Other preparation methods 6 7 Procedure 6 7.1 Specimen set-up . 6 7.2 Specimen soaking. 6 7.3 Back-pressure saturati
16、on. 6 7.4 Consolidation 7 7.5 Permeation. 8 7.6 Final dimensions of the specimen 9 8 Calculation. 9 8.1 Tests at constant head and constant flow rate (Methods A and D). 9 8.2 Falling-head tests 10 9 Test report . 12 Bibliography . 13 BS ISO 17313:2004 Licensed Copy: sheffieldun sheffieldun, na, Sun
17、Nov 26 03:29:48 GMT+00:00 2006, Uncontrolled Copy, (c) BSI IS:31371 O4002(E) iv I SO 4002 All irthgs ersedevr Foreword ISO (the International Organization for Standardization) is a worldwide federation of national standards bodies (ISO member bodies). The work of preparing International Standards is
18、 normally carried out through ISO technical committees. Each member body interested in a subject for which a technical committee has been established has the right to be represented on that committee. International organizations, governmental and non-governmental, in liaison with ISO, also take part
19、 in the work. ISO collaborates closely with the International Electrotechnical Commission (IEC) on all matters of electrotechnical standardization. International Standards are drafted in accordance with the rules given in the ISO/IEC Directives, Part 2. The main task of technical committees is to pr
20、epare International Standards. Draft International Standards adopted by the technical committees are circulated to the member bodies for voting. Publication as an International Standard requires approval by at least 75 % of the member bodies casting a vote. Attention is drawn to the possibility that
21、 some of the elements of this document may be the subject of patent rights. ISO shall not be held responsible for identifying any or all such patent rights. ISO 17313 was prepared by Technical Committee ISO/TC 190, Soil quality, Subcommittee SC 5, Physical methods. BS ISO 17313:2004 Licensed Copy: s
22、heffieldun sheffieldun, na, Sun Nov 26 03:29:48 GMT+00:00 2006, Uncontrolled Copy, (c) BSI IS:31371 O4002(E) I SO 4002 All irthgs ersedevr v Introduction The rate of water flow through the soil is of considerable importance in many aspects of agricultural and urban life. The entry of water into soil
23、, the movement of water to plant roots, the flow of water to drains and wells, and the evaporation of water from the soil surface are but a few of the obvious situations in which the rate of water flow plays an important role. Also in cases of soil pollution and polluted groundwater, prediction of t
24、he rate of movement of soil water is of great importance in obtaining information about the spreading of pollutants. The soil properties that determine the behaviour of soil water flow systems are the hydraulic conductivity and water retention characteristics. The hydraulic conductivity of soil is a
25、 measure of its ability to transmit water. The water retention characteristics are an expression of its ability to store water. These properties determine the response of a soil water system to imposed boundary conditions. BS ISO 17313:2004 Licensed Copy: sheffieldun sheffieldun, na, Sun Nov 26 03:2
26、9:48 GMT+00:00 2006, Uncontrolled Copy, (c) BSI blank 4002:31371 OSI SB Licensed Copy: sheffieldun sheffieldun, na, Sun Nov 26 03:29:48 GMT+00:00 2006, Uncontrolled Copy, (c) BSI INTENRATIONAL TSANDADR IS:31371 O4002(E) I SO 4002 All irthgs ersedevr 1 Soil quality Determination of hydraulic conducti
27、vity of saturated porous materials using a flexible wall permeameter 1 Scope This International Standard specifies a test method for laboratory measurement of the hydraulic conductivity of water-saturated porous materials using a flexible wall permeameter. This International Standard is applicable t
28、o undisturbed or compacted specimens that have a hydraulic conductivity between 1 105 m/s (1 103 cm/s) and 1 1011 m/s (1 109 cm/s). Typical soil types falling in this category are clay, clay and sand tills, silt, peat, mud, etc. 2 Terms and definitions For the purposes of this document, the followin
29、g terms and definitions apply. 2.1 hydraulic conductivity k rate of discharge of water under laminar flow conditions through a unit cross-sectional area of a porous medium under a unit hydraulic gradient and standard temperature conditions (usually 20 C) 2.2 pore volume of flow cumulative quantity o
30、f flow into a test specimen divided by the volume of voids in the specimen 2.3 hydraulic gradient change in total hydraulic head of water per unit distance of flow 3 Significance and use This test method applies to the one-dimensional, laminar flow of water from bottom to top within porous materials
31、 such as soil and rock. The hydraulic conductivity of porous materials generally decreases with an increasing amount of air in the pores of the material. This test method applies to water-saturated porous materials containing almost no air. This test method applies to permeation of porous materials
32、with water. Permeation with other liquids, such as chemical wastes, can be accomplished using procedures similar to those described in this test method. However, this test method is only intended for use when water is the permeant liquid. It is assumed that Darcys law is valid and that the hydraulic
33、 conductivity is essentially unaffected by hydraulic gradient. The validity of Darcys law can be evaluated by measuring the hydraulic conductivity of the specimen at three hydraulic gradients; if all measured values are similar (within about 25 %), then Darcys law may be taken as valid. However, whe
34、n the hydraulic gradient acting on a test specimen is changed, the state of stress will also change, and, if the specimen is compressible, the volume of the specimen will change. Thus, some BS ISO 17313:2004 Licensed Copy: sheffieldun sheffieldun, na, Sun Nov 26 03:29:48 GMT+00:00 2006, Uncontrolled
35、 Copy, (c) BSI IS:31371 O4002(E) 2 I SO 4002 All irthgs ersedevr change in hydraulic conductivity can occur when the hydraulic gradient is altered, even in cases where Darcys law is valid. Normally, hydraulic conductivity measured by laboratory testing is different from large-scale field-test result
36、s. The reason is that samples of the size described in this International Standard are representative for homogeneous soil, but seldom for stratified, fissured or other non-homogeneous soil. In order to obtain results representing the hydraulic conductivity in the field in these cases, large-scale s
37、amples or field-testing shall be considered. 4 Reagents 4.1 Permeant water, as specified by the requester. If no specification is made, tap water shall be used for the permeant liquid. The type of water utilized shall be indicated in the test report. 4.2 De-aerated water. To avoid introducing air, a
38、nd to aid in removing as much air from the test specimen as possible, de-aerated water shall be used. To prevent dissolution of air back into the water, de-aerated water shall not be exposed to air for prolonged periods. 5 Apparatus 5.1 Hydraulic system Constant head (Method A), falling head (Method
39、s B and C), or constant rate of flow (Method D) systems may be utilized provided they meet the criteria outlined as follows. a) Constant head (Method A) The system shall be capable of maintaining constant hydraulic pressure. Pressures shall be measured by a pressure gauge, electronic pressure transd
40、ucer or any other device of suitable accuracy. b) Falling head The system shall allow for measurement of the loss of applied head. The head loss shall be measured with a pressure gauge, electronic pressure transducer, engineers scale, graduated pipette, or any other device of suitable accuracy. Fall
41、ing head tests may be performed with either a constant tail water elevation (Method B) or a rising tail water elevation (Method C). c) Constant rate of flow (Method D) The system shall be capable of maintaining a constant rate of flow through the specimen to within 5 % or better. Flow measurement sh
42、all be by calibrated syringe, graduated pipette, or other device of suitable accuracy. The hydraulic system shall be designed to facilitate rapid and complete removal of free air bubbles from flow lines. The hydraulic system shall have the capability to apply back-pressure to the specimen to facilit
43、ate saturation. The back-pressure may be provided by a compressed gas supply, a deadweight acting on a piston, or any other method capable of applying and controlling the back-pressure to the tolerance required. The above-mentioned test methods are considered equivalent. The accuracy of the test res
44、ults depends on the instruments used. BS ISO 17313:2004 Licensed Copy: sheffieldun sheffieldun, na, Sun Nov 26 03:29:48 GMT+00:00 2006, Uncontrolled Copy, (c) BSI IS:31371 O4002(E) I SO 4002 All irthgs ersedevr 3 5.2 Flow measurement system. Both inflow and outflow volumes shall be measured, unless
45、the lack of leakage, continuity of flow and cessation of consolidation or swelling can be verified by other means. Flow volumes shall be measured by a graduated accumulator, graduated pipette or vertical standpipe in conjunction with an electronic pressure transducer or other column-measuring device
46、 of suitable accuracy. Head losses in the tubes, valves, porous end pieces, and filter paper may lead to error, and shall be less than 10 % of the head loss of the sample. 5.3 System for pressurizing the permeameter cell. The pressurizing system may consist of a reservoir connected to the permeamete
47、r cell and partially filled with de-aerated water, with the upper part of the reservoir connected to a compressed gas supply or other source of pressure. The gas pressure shall be controlled by a pressure regulator and measured by a pressure gauge, electronic pressure transducer or any other device
48、capable of measuring to the tolerance required. A hydraulic system pressurized by deadweight acting on a piston or any other pressure device capable of applying and controlling the permeameter cell pressure to the tolerance required may be used. 5.4 Permeameter cell, in which the specimen and porous
49、 end pieces, enclosed by a membrane sealed to the cap and base, are subjected to controlled fluid pressures. A cell (5) in a typical permeameter system is shown in Figure 1. The permeameter cell may allow for observation of changes in height (lo) of the soil sample. In order to facilitate gas removal, and thus saturation of the hydraulic system, drainage lines lead to the test specimen, to the base and top cap. The drainage lines shall be con