首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献,搜索用时 0 毫秒
1.
Concentrations of 238U, 232Th, 226Ra, 40K and 137Cs are measured in collected soil samples from various locations in the Thrace region of Turkey. The activity concentrations range from 12.82 to 101.75 Bq kg?1 d.w. (dry weight) for 238U, from 5.16 to 73.34 Bq kg?1 d.w. for 232Th, from 185.54 to 5399 Bq kg?1 d.w. for 40K and from 11.42 to 90.73 Bq kg?1 d.w. for 226Ra. In addition to naturally occurring radionuclides, 137Cs activity concentration is determined between 3.05 and 46.78 Bq kg?1 d.w. for soil samples. Determination of the radiological hazard is achieved through calculations of the external terrestrial gamma dose rate in air (nGy h?1) and annual effective dose rate (mSv year?1) and the results are compared with the similar works in different countries.  相似文献   

2.
The radioactivity concentrations of 238U, 226Ra, 232Th and 40K in soil samples around Tarapur vary from 11.5 ± 2.6 to 50.3 ± 6.6, 14.9 ± 0.6 to 40.5 ± 1.2, 18.1 ± 0.4 to 75.0 ± 1.5 and 130.1 ± 1.6 to 295.1 ± 2.6 Bq/Kg respectively. The measured activity concentrations for 238U and 226Ra were compared and found in good agreement with the Indian as well as world average. The average 232Th and 40K concentrations in Tarapur were lower than the Indian average value.  相似文献   

3.
The radioactivity of the 235, 238U and 232Th isotope decay chains for geological samples can usually be assumed to be in equilibrium due to their age. Similarly, one can assume that the isotopic mass proportions are equal to natural isotopic abundance. Current methods used to ascertain activity in these decay chains involve alpha particle spectrometry, ICP-MS or passive gamma-ray spectrometry, all of which can be laborious and time consuming. In this research, we have used thermal and epithermal neutron activation analysis (NAA) of small sample sizes of various geological materials in order to ascertain these activities. By using NAA, we aim to obviate cumbersome sample preparation, the need for large samples and extended counting time. In addition to the decay chains of uranium and thorium, 40K was also determined using epithermal neutron activation analysis to determine total potassium content and then subtracting out its isotopic contribution.  相似文献   

4.

In this paper, three individual models and one generalized radial basis function neural network (RBFNN) model were developed for the prediction of the activity concentrations of primordial radionuclides, namely, 232Th, 238U and 40K. To achieve this, gamma spectrometry measurements of 126 different geological materials were used in the development of the RBFNN models. The results indicated that individual and generalized RBFNN models are quite efficient in predicting the activity concentrations of 232Th, 238U and 40K of geological materials.

  相似文献   

5.
Journal of Radioanalytical and Nuclear Chemistry - To understand the depth wise distribution of the primordial radionuclides, especially in high background radiation areas, their radioactivity...  相似文献   

6.
This work presents the results of 137Cs, 40K, 232Th and 238U concentration (Bq kg−1) values in coastal marine sediments collected from 38 sites along the coastline of the island of Margarita, Venezuela. The purpose was to determine baseline values for these radionuclides in surface marine sediments and to detect if there were any anomalously high concentration values. Only three of the 38 sediments analyzed had measurable values above the detection limit of 0.9 Bq kg−1 for 137Cs and the highest only being 1.4 Bq kg−1. While, the concentration (Bq kg−1) ranges for the primordial radionuclides, 40K, 232Th and 238U were as follows: 12.2–211.7, <1.5–9.8 and <4.4–20.7, respectively. These concentration ranges for the primordial radionuclides can be considered as baseline values for surface marine sediments for areas that are considered not polluted by man or contaminated by nature. Finally, the concentration range of 137Cs can also be employed as baseline values, which only seem to have been the result of the atmospheric testing of nuclear weapons in the past.  相似文献   

7.
8.
9.
Journal of Radioanalytical and Nuclear Chemistry - The aim of this study is to investigate the activity concentrations of 226Ra, 232Th, 40K and 137Cs in soil samples from Seydisehir and Beysehir...  相似文献   

10.
The isomeric yield ratios for134I, for the photofission of232Th and238U with 25-MeV bremsstrahlung have been determined using radiochemical techniques and -spectrometry. Angular moment a of the corresponding fission fragments, Jrms, were calculated by the statistical procedure of Huizenga and Vandenbosch. We have discovered a significant proton odd-even effect on Jrms values, and demonstrated its dependence on the nuclear structure of fragments.  相似文献   

11.
Journal of Radioanalytical and Nuclear Chemistry - On-site 222Rn concentration at three different soil depths was measured at the south-eastern coastal area of Bangladesh to evaluate the annual...  相似文献   

12.
13.
Intake with food and water of the natural radionuclides of the uranium and thorium series was determined for adult population of the south-western region in Poland, where in the 1950-ies an exploration of uranium ore was conducted. Concentration of the radionuclides was determined in food products and drinking water and their annual intake was estimated on the basis of the average annual consumption. The intake of238U,234U and230Th occurred mainly with water (33% to 68%), whereas the intake of232Th,228Th and226Ra was mainly with vegetables, potatoes, milk and flour. From the intake and dose coefficients the annual effective doses from the ingested radionuclides were calculated. The total dose was 5.6 Sv, of which 74% originated from226Ra.  相似文献   

14.
15.
建立了电感耦合等离子体质谱测定水中铀钍元素含量的方法。水样以硝酸酸化处理后直接用电感耦合等离子体质谱法测定,为了消除铀记忆效应对测定结果的干扰,测试溶液的质量浓度以不超过10μg/L为宜,样品测定间隙设置清洗时间为2 min。铀钍元素标准曲线线性相关系数分别为0.999 4,0.999 5;铀、钍的检出限分别为0.000 9,0.002 1μg/L;加标回收率分别为95.70%~112.33%,96.94%~109.98%;测定结果的相对标准偏差分别为0.61%~5.33%,1.16%~1.33%。  相似文献   

16.
Seventeen honey samples collected at different sites during 1992 have been measured using the method of -spectroscopy. Measurements were performed by a low background high purity germanium spectrometer of a relative efficiency of 14.5% and an energy resolution of 1.7 keV. Using natural -ray sources to determine efficiency, it has been shown that out of 17 samples of natural honey only two (of meadow type) have specific activity of137Cs greater than 0.5 Bq kg–1. The remaining samples have the same137Cs concentrations as before May, 1986. Predominant activity in all samples comes from the40K radionuclide, indicating natural honey.  相似文献   

17.
18.
Fallout levels of 137Cs in surface soil from North WesternLibya have been measured using gamma-ray spectrometry. The activity concentrationsof 137Cs in soil ranged from 975 to 1720 mBq . kg —1 . The areal activity concentrations ranged from 1300 to 2250 mBq .m —2 , and were higly correlated with annual precipitation.The effective dose from external exposure to 137Cs is found tobe 3 nSv . y —1 .  相似文献   

19.

The effect of interference and disequilibrium was evaluated in analyzing 238U and 232Th using gamma-ray spectrometry. The interference in 234Th as an indicator of 238U was considerably increased according to the activity level of 232Th compared with that of 238U. However, its correction was necessary to assume that the secular equilibrium in the thorium decay series must be secured in the material. In addition, the disequilibrium in the decay series can be easily shown in the chemical process for manufacturing materials. This makes the limitation in the indirect measurement of natural radionuclides using gamma-ray spectrometry, especially in chemically processed products.

  相似文献   

20.
A232Th source of knowsn disintegration rate and in secular equilibrium was measured to determine the absolute -ray emission intensities of members of its decay chain. Similar measurements were made on sources of highly-enriched235U and of normal uranium metal. The results are compared with values from the literature.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号