Due to the progress of nuclear detection technology and electronic science and technology, one instrument and one sample can simultaneously measure α and β radioactivity, which saves manpower and material resources and brings convenience to work.
Experience has proved that making samples of 0.05 ~ 0. 18 mg/mm2 (generally 0. 1mg/mm2) can not only meet the requirements of measuring α in thick layers (saturated layers greater than the effective thickness) but also meet the requirements of measuring β in thin layers (less than the maximum sampling amount).
For different substances to be tested, the requirement of 0. 1mg/mm2 is not fixed. For example, it is difficult to produce a large amount of solid residues in relatively pure drinking water (although some water samples can be treated with a little more sulfuric acid and precipitated with barium chloride, and more water samples can be taken). Can be relaxed to 0.05mg/mm2 according to the specific situation. For samples with rich sources, the sampling amount can be increased from 0. 15 to 0. 18 mg/mm2, or even 0.3mg/mm2.
Under the condition of pH4, radioactive substances in drinking water samples were precipitated and adsorbed by barium sulfate and activated carbon, and the precipitate was burned to make a sample source of 0.05mg/mm2. Biological sample: the burnt sample ash is made into a sample source of 0.05mg/mm2; Soil sample: Take 0. 1mg/mm2 of treated soil as the sample source, and put it on a low background α and β measuring instrument to measure α and β radioactivity.
It is important to note that when calibrating (calibrating) the instrument (measuring the efficiency of the standard source), the quality of the standard source must be consistent with it, otherwise it will increase the uncertainty of determination.
tool
Low background α, β measuring instrument.
reagent
Sulfuric acid.
muriatic acid
Barium chloride solution (100g/l).
EDTA solution (10g/L).
α source natural uranium powder standard source (specific activity 10Bq/g) or 24 1Am powder standard source (specific activity 10.2Bq/g) and natural uranium (or 239Pu) check the non-point source.
Beta source potassium chloride powder standard source (specific activity 14.4Bq/g) and 90Sr-90Y inspection surface source.
Activated carbon 20g of activated carbon was soaked in 200mLEDTA solution or 200mL( 1+99)HCl, stirred and left overnight. Pour out the supernatant, then filter, wash the activated carbon with water to neutrality, put it in a drying oven and dry it at 105℃.
Sample collection and pretreatment
(1) water sample
Sample collection:
1) When collecting river water, surface water (the first residential water intake point) and main drainage water samples, they should be collected at a certain depth below the water surface; If the water is deep, samples of different depths should be collected at the same time; When the water surface is wide, a few samples should be taken from the left, middle and right of the estuary.
2) Select representative industrial water, tap water and upstream water as control points, and collect samples at the same time.
3) Samples collected from polluted water bodies should be representative, and the collection methods can be divided into three types according to wastewater discharge, wastewater properties, analysis requirements and monitoring purposes: instantaneous collection method, average collection method and individual collection method.
4) The sampling tool can be a glass bottle without radioactive pollution (it is best to use a plastic bucket as the container for water samples), and the sampling bottle (bucket) can be washed with water for many times at the collection site before collection.
5) When collecting in shallow water, be careful not to stir the mud at the bottom of the water.
6) Sampling bottles (barrels) must have fixed numbers and be earmarked for special purposes to prevent cross-contamination.
7) The sampling amount (volume) depends on the analysis item, generally 2 ~ 10L, and the gap of110 should be ensured in the container; Under no circumstances can the container be filled with water samples.
Sample pretreatment:
Sampling records and sample labels should be filled in when sampling, and the collected water samples should be acidified with nitric acid or hydrochloric acid immediately (acidification pH ≤ 2); After standing for 24 hours, the supernatant was taken for analysis (except radon measurement).
If the water sample is turbid, it should be filtered before acidification.
(2) Soil samples
Sample collection:
Soil sampling sites should be selected in a flat place and distributed appropriately according to needs. Diagonal sampling method and plum blossom sampling method should be adopted when sampling. According to different monitoring purposes, the sampling depth is 5cm. When sampling, draw a square of 10cm× 10cm with a knife, and take out the soil sample with a vertical depth of 5cm; Take the soil below 20cm for the deep soil.
In order to collect contaminated soil samples, the natural conditions, agricultural production environment, soil properties and pollution history of the investigation area were investigated at first. On this basis, sampling points are set as needed to represent the pollution situation of a certain area, and an unpolluted area is selected as a control.
Samples of river bottom silt should be collected in the same place as water samples for comparison.
Sample pretreatment:
Wrap the soil (river bottom mud) samples collected on site with cleaning paper (plastic bag) or put them in other clean containers, and indicate the sampling time, place, sampling area, depth and the surrounding conditions of the sampling point.
Natural drying of soil samples in the laboratory, or drying at 1 10℃, removing impurities such as stones and grass, and weighing.
Put the dried soil sample on a clean flat plate and grind it into a square with a thickness of 1 ~ 2 cm. Draw a crosshair along the diagonal of the square and divide the sample into four parts. Draw a square with the intersection of intersecting lines as the center, and remove all the soil outside the square. Repeatedly eliminate until the residual soil sample reaches about 300g, put the soil sample into a high-temperature furnace and burn it at 500℃ for1~ 2 hours. After cooling, it is ground in a mortar, sieved with a 40 ~ 100 mesh sieve, mixed evenly, and bottled for inspection.
(3) Biological samples
Vegetables:
Remove the roots of the collected vegetable samples, wash them, and weigh the fresh samples after the surface moisture is completely dried or dried. Chop fresh samples, air-dry or put them in a blast drying box, put the dried samples in a porcelain evaporating dish and carbonize them in an electric furnace. In the process of carbonization, prevent the sample from catching fire, so that some ash particles in the sample are taken away by hot air and cause losses. And then transferred to a high-temperature furnace, the temperature is gradually increased from low to 400-450 DEG C, and the sintering is often observed to prevent. Completely ashed ash powder should be gray and loose. If the ash powder is still black, it should be taken out, cooled, wetted and evaporated with 6mol/LHNO3 or 6mol/LNaNO2 solution, and then ashed again.
Put the completely ashed sample at room temperature, weigh the ash mass and save it for later use.
Rice:
In the morning and evening harvest season, the paddy fields that must be monitored are selected, and about 500g mixed samples are collected from different parts to understand the situation of irrigation and fertilization (especially potassium fertilizer) in paddy fields. Remove impurities from the collected rice samples, weigh fresh samples, moisten the samples with 30g/LNaAc solution, put them in a porcelain evaporating dish, carbonize them in an electric furnace, and then transfer them to a high-temperature furnace for ashing at 450℃. The completely ashed ash powder should be grayish white. If the ashing is not complete, 6 mol/L nano _ 2 solution can be used to treat the vegetable samples, re-ashing and storing for later use.
Fish samples:
Dissect fish samples captured in polluted river sections (or control points), remove scales and internal organs, wash, dry or dry in the sun, and weigh a certain amount of fish meat and bones from each fish (if there are only small fish, it is not necessary to analyze fish meat and bones separately).
Chop the dried fish samples respectively, put them into a weighed porcelain evaporating dish, carbonize them on an electric furnace, and then transfer them to a high-temperature furnace when there is no smoke. Gradually raise the temperature, and finally keep it at about 450℃ until it becomes loose gray ash. After cooling to room temperature, weigh the ashes and keep them for later use.
Meat samples:
After removing bones and internal organs, make samples according to the preparation method of fish samples for later use.
Sample preparation, measurement and result calculation
Water sample: the prepared solid residue powder was weighed as 0.05mg/mm2.
Soil sample: the weight of the treated powder is 0. 1mg/mm2.
Biological sample: weigh the prepared ash to 0.05 mg/mm2.
Spread the above-mentioned weighed samples evenly in the sample tray, and then make formal measurement after checking the instrument with surface standard source. Measure the α and β counting rates, measure the background, and find out their respective net counting rates. According to different quality requirements, find out the standard source efficiency of corresponding quality and calculate α and β radioactivity.
Result calculation
The total α and β radioactivity in water, soil and living things are calculated by formulas [(66.60), (66.63)], [(66.6 1), (66.65)] and [(66.62), (66.66)] respectively.
When the total beta radioactivity in mineral water is greater than 1.0Bq/L, the total beta radioactivity in food (organism) should be reduced by 40K, and the calculation method is shown in formula (66.64).
References and reference materials
Chen Yingqiang, Zhang Qingwen, Lin Chao, et al. Determination of 23 1pa in the 227th geological sample [J]. Uranium Geology, 3(5):3 14-3 18.
Zhiheng Chen. 1982. General formula for measuring radon (thorium) concentration by balloon method [J]. Journal of Fudan University (Natural Science Edition), 2 1(3):284-292.
Chu, Guo Chunhua. 2003. Progress of Thermoionization Mass Spectrometry in Earth Science [J]. Modern Instruments, (1):7- 1 1.
Cui. 2004. Indoor environmental testing instruments and application technology [M]. Beijing: Chemical Industry Press.
Dai Honggui 1992. caso4: development and properties of TM PTFE thermoluminescent sheet [J]. bulletin of nuclear agriculture, 13 (supplement): 24 1-244
Determination of radioactivity ratios of 234U/238U, 230th and 232T in geological samples (GB/T1307-91) [S].1991. Beijing: China Standards Publishing House.
Fangfang, Jia. 1999. principle and application of α-cup radon measurement method [J]. geophysical and geochemical exploration, 22(4):2 18-222
Code for Quality Assurance of Radioactive Mineral Analysis and Testing Laboratories (EJ/T 751-1993) [S].1993: China Standards Publishing House.
Fu Jin, Han, Zhang Biao. 2003. Measurement of radon exhalation rate in uranium tailings by activated carbon adsorption method [J]. Radiation Protection Newsletter, 23(2):32-35.
Gong Yuecun, Liu Zongyuan. 1992. application of passive thermoluminescence radon accumulation detector [J]. radiation protection, 12( 1):75-78
Han Jun, Fu Zhonghua, Mao Xingen, et al. 2004. Quantitative analysis of plutonium in environmental samples by isotope dilution mass spectrometry [J]. Nuclear Chemistry and Radiochemistry, 26( 1):6 1-64.
Hou, Dai Jun and Chen. 2005. Measurement Technology and Quality Control of TLD [J]. nuclear electronics and Detection Technology, 25(6):772-777.
Hu,,,. 199 1. Error estimation of deducting cosmic ray response method in ground gamma radiation dose rate measurement [J]. Radiation protection, 1(6):444.
Gamma radioactive air absorbed dose rate meter for environmental monitoring (jjg521-88) [s].1988. Beijing: China Metrology Press.
Jia, Xu Biwen,, et al. Development of Portable Atmospheric Pressure Air Pulse Ionization Chamber Radiometer [J]. Journal of Geophysics, 33(3):356-36 1.
Radionuclide limit of building materials (GB 6566—2001) [s] .2001. Beijing: China Standards Publishing House
Gao Dongchu, Liu, et al. 2004. Technical transformation of FD- 105K radon meter and development of its calibrator [J]. Northeast Earthquake Research, 20(2):23-28
Jin Zhongfan, Yin Weimin, Niu Feng, et al. 2000.FD- 105K common fault analysis and solutions [J]. Northeast Earthquake Research, 16(2):22-25.
Li Deping, Pan Qiangzi. 1988. handbook of radiation protection (volume 2) [M]. Beijing: Atomic Energy Press.
Li huaxian 1994. A new technological breakthrough in the dating of unbalanced uranium series-high-precision and high-sensitivity 238 u-234 u-230t isotope mass spectrometry and its application [J]. Progress in Earth Science, 9(3):79-85
Li Hongxing. 198 1. basics of radiation protection [M]. Beijing: Atomic Energy Press, 276.
Lin Lianqing, Ren Tianshan, Li Guiyun. 1986. Research on passive indoor accumulation detector of activated carbon [J]. Radiation protection, 6( 1): 1.
Guofan Liu, Song Jinlian, Wang,, et al. Measurement of radon concentration in air by electrostatic collection-solid track etching method [J]. Radiation protection, 14(3):234-237
Liu jianfen 2000. Test of detection efficiency correction coefficient for total β measurement of soil samples [J]. Isotope, 13(2):92-96
Liu Shutian, Xia Yihua. 1997。 Practical handbook of environmental pollution monitoring [M]. Beijing: Atomic Energy Press, 52.
Long, Jia Baoting, et al. 2005. Mass spectrometry analysis technology of sub-pik plutonium. See: Proceedings of the 2005 National Symposium on Inorganic Mass Spectrometer, Isotope Mass Spectrometer and Mass Spectrometer [C]. Beijing: Atomic Energy Press.
Peng Zicheng. 1997. New technology of Quaternary dating-new development of uranium series method by thermal ionization mass spectrometry [J]. Quaternary research, (3): 258-264.
γ -ray energy spectrum analysis method for radionuclides in biological samples (GB/T16145-1995) [S].1995. Beijing: China Standards Publishing House.
γ -ray energy spectrum analysis method for radionuclides in water (GB/T1640—1995) [S].1995. Beijing: China Standards Publishing House.
Tian Zhiheng, left, small. 1993. radon measurement by electret and its application [J]. atomic energy science and technology, 27( 1):57-6 1.
γ -ray spectrum analysis method of radionuclides in soil [S] (GB11743-89)1989. Beijing: China Standards Publishing House.
Wang Bin. 2005. Development of radon detection standard device [D]. Sichuan: Chengdu University of Technology.
Wang Qiang. 2006. Application of high purity germanium γ -ray spectrometer in analysis of uranium geological samples. See: Proceedings of the Symposium on Geological Analysis and Testing Technology and Quality Management in Nuclear Industry (2006) [c]. Beijing: Beijing Institute of Geology, Nuclear Industry.
, process,. 2005. Discussion on determination method of total α and total β radioactivity in drinking water [J]. Water purification technology, 24(3):7 1-76.
Wei Gangjian, Li,,, et al. Preliminary Study on Thermoelectric Ionization Mass Spectrometry (TIMS)U-Th Dating and Its Application [J]. Geochemistry, 26(2):68-74.
Wei suya 1992. performance test of two improved radon samplers [r]. annual report of China institute of radiation protection, 9
Wu Huishan, Lin Yufei, Bai Yunsheng, et al. 1995. Radon measurement method and its application [M]. Beijing: Atomic Energy Press.
Wu, Guo Dongfa, Lin Chao, et al. 2005. Application of analytical testing technology to in-situ leaching sandstone-type uranium deposits [R]. Beijing: Beijing Institute of Geology, Nuclear Industry, 19 1-2 13.
Xia. 1992. lead isotope method in uranium exploration [M]. Beijing: atomic energy press.
Yang ailan 1995. monitoring method of β content in food [J]. radiation protection communication, 15(3):43-46.
Yang Yaxin, Wu Yamei, Peng Nie, et al. A method for measuring radon exhalation rate in the environment [J]. Journal of East China Institute of Geology, 24( 1):37-40
Test method for drinking natural mineral water (GB/T 8538-1995) [s].1995. Beijing: China Standards Publishing House.
Zhang Guohua, Fang Fang, Geng Bo. 2005. Development of α radon meter in KZ-D02F ionization chamber [J]. nuclear electronics and Detection Technology, 25(6):704-708.
Zhang Huaiqin, Su Jingling, Yao Wanyuan, et al. 1989. Portable monitor for measuring radon and its daughters in air by accumulation method [J]. Radiation Protection, 9(6):438-442.
Zhang Wentao, Jin Jiekun, Gong Xinyu, et al. 2003. Study on monitoring method of radon emission from building materials [J]. industrial health and occupational diseases, 29(4):206-2 1 1.
Zhang Zhaofeng, Peng Zicheng, He Jianfeng, et al. Factors to be considered in dating uranium series by thermal ionization mass spectrometry [J]. Acta Mass Spectrometry, 22(3): 1-7
Zhao, Wang Jun, Lu Baikeng, et al. Application of isotope dilution mass spectrometry in chemometrics [J].Acta mass spectrometry,19 (2):16-21.
Zhao, Wang Jun 1996. Determination of Antimony Atomic Weight by Absolute Mass Spectrometry [J].Acta Metrology, 17(2):8 1-84.
Zhao Yunlong, Gu Dingxiang, Li Ronghui, et al. 1999. Determination of the 230th specific activity in uranium ore by activity ratio dilution method [J]. Science Bulletin, (14):103-105.
Zhao Guizhi and Xiao Todd. 2009. Reconstruction and measurement method of α spectrum data of 222Rn and 220Rn in air [J]. Nuclear technology, 32 (6):111.
Zhou Tao, Zhao, Wang Jun, et al. 2006. Application progress of isotope mass spectrometry and inorganic mass spectrometry in chemometrics. See: 2006 World Chinese Mass Spectrometry Symposium and Proceedings of the 8th National Symposium of China Mass Spectrometry Society [C].
Change H w 198 1. Application of passive interaction radon monitor in environmental monitoring [J]. Health Physics, 40: 693
á tmc1380-97: Standard test method for determination of uranium content and isotope composition by isotope dilution spectrometry [J]; Yearbook of ASTM standards. 2004. 12 ( 1) : 8 15 - 8 17
Edwards R L, Chen J H, Wasserburg G J.1996/1997.238U-234U-230T-232 Systematic and accurate measurement of the past 500,000 years [J]. Earth and Planetary Science Letter, 81:/Kloc
Gu Zhiying, Lalade, Liu Tiesheng. Sedimentary weathering history of loess in China based on uranium, thorium series nuclides and cosmogenic beryllium [J]. Journal of Geochemistry, 61:5221-5231
Harbottle G, Evans C v. 1997. Methods for γ -ray determination of natural and man-made radionuclides in environmental and soil science [J]. Radioactivity and Radiochemistry, 8 (1): 38-46
IAEA. 2003. Support technology and equipment [M]. Vienna: IAEA
Lucas H f 1957. Review of scientific instruments [J], 28: 680
Dao Guo Shi Mo. 1987. Comparison of different instruments for measuring radon concentration in the air. The appearance of radon and its decay products. Attribute and health impact [M]. Edited by Philip K. Hope, 160-17 1
Pierre Sidon 1964. Radiological health and safety in nuclear material processing [M]. Vienna: IAEA, 848
Graphite m 1985. A mobile ionization chamber [M] for measuring radon concentration in the atmosphere, radon family in the atmosphere and environmental radioactivity. Okada: Japan Atomic Energy Association, Tokyo, 37-42
[2] the diurnal variation of radon -222 concentration in residential buildings of Speidi. H. b. grand junction [M]. cole radon EC HA SL-287, USA
Stephen Wolfe. 1999. analytical methods of uranium in geological environment materials [J]. mineralogical review, 38: 627 -634
Thomas J w 1970. Study on Radon by Double Filter [J]. Healthy,11:113
This chapter was written by Guo Dongfa (Analysis and Testing Center of Beijing Institute of Geology, Nuclear Industry).
Li Yaping, Ni Chuanzhen, Li Jiasheng, Deng Xiuwen and Yan Shidong (Guangdong Institute of Mineral Application).