ImageVerifierCode 换一换
格式:PDF , 页数:22 ,大小:1.18MB ,
资源ID:585258      下载积分:10000 积分
快捷下载
登录下载
邮箱/手机:
温馨提示:
如需开发票,请勿充值!快捷下载时,用户名和密码都是您填写的邮箱或者手机号,方便查询和重复下载(系统自动生成)。
如填写123,账号就是123,密码也是123。
特别说明:
请自助下载,系统不会自动发送文件的哦; 如果您已付费,想二次下载,请登录后访问:我的下载记录
支付方式: 支付宝扫码支付 微信扫码支付   
注意:如需开发票,请勿充值!
验证码:   换一换

加入VIP,免费下载
 

温馨提示:由于个人手机设置不同,如果发现不能下载,请复制以下地址【http://www.mydoc123.com/d-585258.html】到电脑端继续下载(重复下载不扣费)。

已注册用户请登录:
账号:
密码:
验证码:   换一换
  忘记密码?
三方登录: 微信登录  

下载须知

1: 本站所有资源如无特殊说明,都需要本地电脑安装OFFICE2007和PDF阅读器。
2: 试题试卷类文档,如果标题没有明确说明有答案则都视为没有答案,请知晓。
3: 文件的所有权益归上传用户所有。
4. 未经权益所有人同意不得将文件中的内容挪作商业或盈利用途。
5. 本站仅提供交流平台,并不能对任何下载内容负责。
6. 下载文件中如有侵权或不适当内容,请与我们联系,我们立即纠正。
7. 本站不保证下载资源的准确性、安全性和完整性, 同时也不承担用户因使用这些下载资源对自己和他人造成任何形式的伤害或损失。

版权提示 | 免责声明

本文(BS ISO 17155-2012 Soil quality Determination of abundance and activity of soil microflora using respiration curves《土质 采用呼吸曲线对土壤微植物群的丰度和活性的测定》.pdf)为本站会员(rimleave225)主动上传,麦多课文库仅提供信息存储空间,仅对用户上传内容的表现方式做保护处理,对上载内容本身不做任何修改或编辑。 若此文所含内容侵犯了您的版权或隐私,请立即通知麦多课文库(发送邮件至master@mydoc123.com或直接QQ联系客服),我们立即给予删除!

BS ISO 17155-2012 Soil quality Determination of abundance and activity of soil microflora using respiration curves《土质 采用呼吸曲线对土壤微植物群的丰度和活性的测定》.pdf

1、raising standards worldwideNO COPYING WITHOUT BSI PERMISSION EXCEPT AS PERMITTED BY COPYRIGHT LAWBSI Standards PublicationBS ISO 17155:2012Soil quality Determinationof abundance and activity ofsoil microflora using respirationcurvesBS ISO 17155:2012 BRITISH STANDARDNational forewordThis British Stan

2、dard is the UK implementation of ISO 17155:2012. Itsupersedes BS ISO 17155:2002 which is withdrawn.The UK participation in its preparation was entrusted to TechnicalCommittee EH/4, Soil quality.A list of organizations represented on this committee can beobtained on request to its secretary.This publ

3、ication does not purport to include all the necessaryprovisions of a contract. Users are responsible for its correctapplication. The British Standards Institution 2012. Published by BSI StandardsLimited 2012ISBN 978 0 580 71396 5ICS 13.080.30Compliance with a British Standard cannot confer immunity

4、fromlegal obligations.This British Standard was published under the authority of theStandards Policy and Strategy Committee on 31 October 2012.Amendments issued since publicationDate Text affectedBS ISO 17155:2012 ISO 2012Soil quality Determination of abundance and activity of soil microflora using

5、respiration curvesQualit du sol Dtermination de labondance et de lactivit de la microflore du sol laide de courbes de respirationINTERNATIONAL STANDARDISO17155Second edition2012-10-01Reference numberISO 17155:2012(E)BS ISO 17155:2012ISO 17155:2012(E)ii ISO 2012 All rights reservedCOPYRIGHT PROTECTED

6、 DOCUMENT ISO 2012All rights reserved. Unless otherwise specified, no part of this publication may be reproduced or utilized in any form or by any means, electronic or mechanical, including photocopying and microfilm, without permission in writing from either ISO at the address below or ISOs member

7、body in the country of the requester.ISO copyright officeCase postale 56 CH-1211 Geneva 20Tel. + 41 22 749 01 11Fax + 41 22 749 09 47E-mail copyrightiso.orgWeb www.iso.orgPublished in SwitzerlandBS ISO 17155:2012ISO 17155:2012(E) ISO 2012 All rights reserved iiiContents PageForeword iv1 Scope 12 Nor

8、mative references . 13 Terms and definitions . 14 Principle . 25 Reagents 26 Apparatus 27 Sampling 37.1 Sample quantities 37.2 Sampling and storage 37.3 Soil sample characteristics 48 Procedure 48.1 Test 48.2 Toxicity testing . 49 Calculation 59.1 Microbial parameters 59.2 Interpretation of data 610

9、 Test report . 8Annex A (informative) Results of a laboratory ring test carried out in Germany 9Annex B (informative) Comparison of microbial biomass determination by respiration curve measurement (this International Standard) and substrate-induced respiration (ISO 14240-11) 11Bibliography .13BS ISO

10、 17155:2012ISO 17155:2012(E)ForewordISO (the International Organization for Standardization) is a worldwide federation of national standards bodies (ISO member bodies). The work of preparing International Standards is normally carried out through ISO technical committees. Each member body interested

11、 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 in the work. ISO collaborates closely with the International Electrotechnical Comm

12、ission (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 prepare International Standards. Draft International Standards adopted by the technical

13、 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 some of the elements of this document may be the subject of patent rights. ISO shall

14、not be held responsible for identifying any or all such patent rights.ISO 17155 was prepared by Technical Committee ISO/TC 190, Soil quality, Subcommittee SC 4, Biological methods.This second edition cancels and replaces the first edition (ISO 17155:2002), which has been technically revised.iv ISO 2

15、012 All rights reservedBS ISO 17155:2012INTERNATIONAL STANDARD ISO 17155:2012(E)Soil quality Determination of abundance and activity of soil microflora using respiration curves1 ScopeThis International Standard specifies a test method for determining the activity of active aerobic, heterotrophic mic

16、robial biomass in soils. This method is applicable to the monitoring of soil quality and to the evaluation of the ecotoxic potential of soils and soil materials. It is also applicable for soils sampled along contamination gradients in the field and to soils that are contaminated experimentally in th

17、e field or in the laboratory.2 Normative referencesThe following referenced documents are indispensable for the application of this document. For dated references, only the edition cited applies. For undated references, the latest edition of the referenced document (including any amendments) applies

18、.ISO 10381-6, Soil quality Sampling Part 6: Guidance on the collection, handling and storage of soil under aerobic conditions for the assessment of microbiological processes, biomass and diversity in the laboratoryISO 10390, Soil quality Determination of pHISO 10694, Soil quality Determination of or

19、ganic and total carbon after dry combustion (elementary analysis)ISO 11277, Soil quality Determination of particle size distribution in mineral soil material Method by sieving and sedimentationISO 11465, Soil quality Determination of dry matter and water content on a mass basis Gravimetric methodISO

20、 14238, Soil quality Biological methods Determination of nitrogen mineralization and nitrification in soils and the influence of chemicals on these processes3 Terms and definitionsFor the purposes of this document, the following terms and definitions apply.3.1basal respiration rateRBconstant mass of

21、 CO2released or mass of O2consumed per unit mass of soil per unit time without substrate additionNOTE See Figure 1 for a typical basal respiration curve.3.2substrate-induced respiration rateRSconstant mass of CO2released or mass of O2consumed per unit mass of soil per unit time shortly after additio

22、n of a carbon substrateNOTE 1 See Figure 1 for a typical substrate-induced respiration curve.NOTE 2 If glucose is used as a carbon substrate, microbial biomass can be determined from the substrate-induced respiration rate (see ISO 14240-11). ISO 2012 All rights reserved 1BS ISO 17155:2012ISO 17155:2

23、012(E)3.3respiratory activation quotientQRbasal respiration rate divided by substrate-induced respiration rateQRRRBS= (1)3.4specific growth rateexponent representing respiration rate per unit of time during the exponential phase of growthNOTE See Equation (3).3.5time to the peak maximumtpeakmaxtime

24、from addition of substrate to the maximum respiration rateNOTE 1 See Figure 1.NOTE 2 The time to the peak maximum also reflects the viability of the growing organisms.3.6cumulative CO2evolution or O2consumptionCRtotal area bounded by the line of the soil respiration rate curve to the time axis from

25、time of the addition of substrate to the time of peak maximum (tpeakmax)NOTE See Figure 1.3.7soil materialmaterial composed of excavated soil, dredged materials, manufactured soils, treated soils or fill materials4 PrincipleThe CO2production or O2consumption (respiration rate) from unamended soils a

26、s well as the decomposition of an easily degraded substrate (glucose + ammonium + phosphate) is monitored regularly (e.g. every hour). From the CO2production or O2consumption data, the different microbial parameters (basal respiration, substrate-induced respiration, respiratory activation quotient,

27、tpeakmax, CR) can be calculated.5 Reagents5.1 Glucose, C6H12O6.5.2 Potassium dihydrogenphosphate, KH2PO4.5.3 Diammonium sulfate, (NH4)2SO4.5.4 Substrate, consisting of a mixture of 80 g of glucose (5.1), 13 g of diammonium sulfate (5.3), and 2 g of KH2PO4(5.2), which is thoroughly ground and mixed i

28、n a mortar.6 ApparatusOrdinary laboratory equipment and 6.1.2 ISO 2012 All rights reservedBS ISO 17155:2012ISO 17155:2012(E)6.1 Respirometer for continuous measurement of CO2evolution or O2consumption, maintained at a constant temperature (preferably 20 C). Suitable examples of equipment are given i

29、n ISO 16072.2KeyX t h timeY R g g1dmh1CO2or O2 respiration ratesCRcumulative CO2evolution or O2consumptiondp/dt rate of product formation after substrate additionK respiration rate of K-strategist at the time of substrate additionr respiration rate of r-strategist at the time of substrate additiontp

30、eakmaxtime to the peak maximum specific growth rate1 RSsubstrate-induced respiration RS= K + r (at t = 0)2 RBbasal respiration 3 substrate additionFigure 1 Soil respiration rate before and after addition of an easily degraded substrate7 Sampling7.1 Sample quantitiesChoose the size of the soil sample

31、s taking into account the apparatus (6.1) used, the organic matter content of the samples (7.3) and the soil needed for sample characterization (7.3). It is recommended that at least three replicates per sample be measured.7.2 Sampling and storageThe recommendations in ISO 10381-6 for collection, ha

32、ndling and storage of soil samples shall be followed. ISO 2012 All rights reserved 3BS ISO 17155:2012ISO 17155:2012(E)7.3 Soil sample characteristicsSoil samples generating soil respiration curves can be obtained from mineral, organic, polluted, and unpolluted soils. Determine the following characte

33、ristics for each soil sample: particle size distribution in accordance with ISO 11277; water content in accordance with ISO 11465; water-holding capacity in accordance with Annex A of ISO 14238:2012; pH in accordance with ISO 10390; organic matter content in accordance with ISO 10694.8 Procedure8.1

34、TestPre-incubate moist soil samples (preferably 40 % to 60 % of maximum water holding capacity or 0,01 MPa to 0,03 MPa suction pressure) at 20 C for 3 d to 4 d before the beginning of the measurement. Measure the basal respiration of the sub-samples first. Measure the respiration rates until constan

35、t rates are obtained.After measuring the basal respiration, add 10 mg of the substrate (5.4) per gram soil (dry mass) and mix homogeneously with a spatula into the soil samples. If the organic matter content is 5 %, add 0,2 g of the substrate per gram humus (see References 45).8.2 Toxicity testingIn

36、 principle, testing the influence of chemicals should also be possible with the method. Up to the time of publication, there is only scarce experience available in the literature.To determine the influence of chemicals on the abundance and activity of soil microorganisms, a soil with low content of

37、organic carbon (mass fraction between 0,5 % and 1,5 %). Particles of size 0,3 (mineral soils arable, grassland), QR 0,4 (mineral forest soils) and QR 0,6 (organic layers L, Of, Oh) and tpeakmax 50 h are indicative for polluted materials (see References 7 and 8).Moreover, polluted samples often do no

38、t show any logarithmic increase of respiration rates after addition of substrate and/or formation of double peaks (see Figure 2). Double peak formation is caused by a short-term or selective toxic effect of a contaminant. In particular, slowly growing fungi with the marker 18:29,12 seem to be respon

39、sible for the formation of a second respiration maximum (Reference 15).NOTE Double peaks can also occur in unpolluted samples. Reasons for this phenomenon are growth of fungi due to suboptimal (high) water contents. 6 ISO 2012 All rights reservedBS ISO 17155:2012ISO 17155:2012(E)KeyX t h timeY R g g

40、1dmh1CO2respiration rateCRcumulative CO2evolution or O2consumptionRSsubstrate-induced respirationtpeakmaxtime to the peak maximum1 unpolluted soil (control), Reference 42 Cu-polluted soil (190 mg kg1dm), Reference 53 TNT-polluted soil (50 mg kg1dm), Reference 64 substrate additionaReference 1.bRefer

41、ence 2.cReference 2.Figure 2 Soil respiration curves of an unpolluted and two polluted soils9.2.2 Additional criteria for the interpretation of the results from soils deliberately contaminated with chemicalsTheoretically, when a chemical is added to soil, the micro-flora can respond in four differen

42、t ways, of which the two intermediate are most likely to occur. Death: the substance is very toxic. The respiration decreases rapidly, but if the toxic substance is removed, either by degradation or evaporation, the survivors can decompose the dead biomass and the respiration is temporarily as high

43、or higher than before the addition of the substance, but the biomass remains low for a considerable time (see Reference 10). Intolerance: the toxicity of the test substance is moderate. Sensitive species are replaced by more resistant ones. The decomposition of soil organic matter becomes less effic

44、ient and less biomass is formed (see Reference 11). The activity and vitality of the microorganisms might also be reduced. ISO 2012 All rights reserved 7BS ISO 17155:2012ISO 17155:2012(E) No observed effect: the toxicity of the test substance is small. If some species are affected they are replaced

45、by others that are as effective as the original flora (see Reference 12). CO2from the slow degradation of an organic test substance can possibly mask a reduced degradation of soil organic matter. Enhancement: the test substance is a suitable substrate for at least some of the soil organisms. Respira

46、tion is increased until the test substance is consumed (see Reference 13). The biomass and vitality of the growing organisms are also increased.The responses of intolerance or no observed effect to a chemical are the most likely to occur.10 Test reportThe test report shall include the following info

47、rmation:a) general: soil collection, treatment, incubation, including date collected, length of storage, temperature of storage, test substance: chemical identification data (chemical testing), soil characteristics (see also 7.3): particle size distribution in accordance with ISO 11277 water content

48、 in accordance with ISO 11465 water-holding capacity in accordance with Annex A of ISO 14238:2012; pH in accordance with ISO 10390 organic matter content in accordance with ISO 10694;b) test conditions: date and place of sampling, date of start and end of the test, temperature, incubation time with

49、the test substance before microbial measurements, concentrations tested or range of concentrations in test area compared to background levels, solvent used to add the test substance;c) results: list of the microbial parameters for each sub-sample, mean values for each sample, plot of log of concentration of test substance vs. microbial parameters, EC10and EC50, regression of these relationships.8 ISO 2012 All rights reservedBS ISO 17155:201

copyright@ 2008-2019 麦多课文库(www.mydoc123.com)网站版权所有
备案/许可证编号:苏ICP备17064731号-1