矿井水中天然总α放射性的混凝处理技术研究

本文研究了混凝沉淀工艺处理矿井水中天然总α放射性核素铀、镭的技术和条件,通过选择适当的混凝剂、加药量、pH值等条件可将铀的去除率提高到80％左右,使用铀专用混凝剂MHU则可使铀的去除率达到87％。对于镭的去除不能单纯依靠铀混凝剂MHU,尚需添加镭的吸附助剂MHR,则可使镭的去除率提高到80％以上。该工艺的最大优点在于充分利用了煤矿现存的大量矿井水悬浮物处理设施,大大节省了新建工程的投资费用,而且新增加的药剂费用不足0.1元/t水,可在煤矿推广应用。     

抽水蓄能电站建设中注意防止氡污染

针对某抽水蓄能电站地下勘探平洞检测氡气浓度超标问题,分析氡污染危害,提出防止氡污染的措施。     

放射性废物桶内干燥整备研究进展

桶内干燥具有很高的减容比,已经逐渐被国外核电站用来处理放射性废液,为我国核电废物贮存和处理提供了一条新的途径。详细介绍了电加热、热风加热和微波加热3种桶内干燥装置的研究应用实例,主要内容包括干燥装置的过程控制、干燥产量(蒸发速率和进料速率)、干燥产物的含水率和减容比。通过分析对比得出,电加热和热空气加热型装置投入产出高,但仅适合流动和传热好的废物整备;微波加热型装置前期投入大,适用却更广,尤其适合底泥等一类含有有机物质的废物。     

Measurement of gross alpha and gross beta activity concentrations in human tooth

The gross alpha and gross beta activity concentrations were measured in human tooth taken from 3 to 6 age-groups to 40 and over ones. Accumulated teeth samples are investigated in two groups as under and above 18 years. The gross alpha and beta radioactivity of human tooth samples was measured by using a gas-flow proportional counter (PIC-MPC 9604-α/β counter). In tooth samples, for female age-groups, the obtained results show that the mean gross alpha and gross beta activity concentrations varied between 0.534-0.203 and 0.010-0.453 Bq g⁻¹ and the same concentrations for male age-groups varied between 0.009-1.168 and 0.071-0.204 Bq g⁻¹, respectively.     

A method for determining the analytical form of a radionuclide depth distribution using multiple gamma spectrometry measurements

When characterizing environmental radioactivity, whether in the soil or within concrete building structures undergoing remediation or decommissioning, it is highly desirable to know the radionuclide depth distribution. This is typically modeled using continuous analytical expressions, whose forms are believed to best represent the true source distributions. In situ gamma ray spectroscopic measurements are combined with these models to fully describe the source. Currently, the choice of analytical expressions is based upon prior experimental core sampling results at similar locations, any known site history, or radionuclide transport models. This paper presents a method, employing multiple in situ measurements at a single site, for determining the analytical form that best represents the true depth distribution present. The measurements can be made using a variety of geometries, each of which has a different sensitivity variation with source spatial distribution. Using non-linear least squares numerical optimization methods, the results can be fit to a collection of analytical models and the parameters of each model determined. The analytical expression that results in the fit with the lowest residual is selected as the most accurate representation. A cursory examination is made of the effects of measurement errors on the method.     

云南临沧盆地土壤天然放射性测定及环境影响评价

临沧盆地受其基底花岗岩的影响,环境中存在天然放射性水平异常。本文测得其土壤中放射性核素226Ra、238U、232Th和40K的比活度分别为53.4(38.7-62.8)、161.2(127.3-211.7)、120.9(106.5-140.6)和632.2(521.7-707.5)Bq/kg,明显高于全国和世界平均值。花岗岩天然放射性水平较高,与土壤放射性有一定的相关性,为土壤伴生放射性提供了较好的来源。采用测得的土壤放射性核素226Ra、232Th和40K的比活度,计算了距地面1m高处空气中γ辐射吸收剂量率和年有效剂量率,并对γ辐射外照射水平进行了评价。评价结果表明,虽然该区的空气吸收剂量率较高,但是年有效剂量率在容许范围之内。因此该区属于外照射水平的安全区域,人居环境不受影响。     

Use of Natural 35S to Trace Sulphate Cycling in Small Lakes,Flattops Wilderness Area,Colorado, U.S.A.

Measurements of the cosmogenically-produced ³⁵S, a radioisotope of sulphur (t_1/2 = 87 days), are reported for the Ned Wilson Lake watershed in Colorado. The watershed contains two small lakes and a flowing spring presumed to be representative of local ground water. The watershed is located in the Flattops Wilderness Area and the waters in the system have low alkalinity, making them sensitive to increases in acid and sulphate deposition. Time series of ³⁵S measurements were made during the summers of 1995 and 1996 (July–September) at all three sites. The system is dominated by melting snow and an initial concentration of 16–20 mBq L^-1 was estimated for snowmelt based on a series of snow samples collected in the Rocky Mountains. The two lakes had large initial ³⁵S concentrations in July, indicating that a large fraction of the lake water and sulphate was introduced by meltwater from that year's snowpack. In 1995 and 1996, ³⁵S concentrations decreased more rapidly than could be accounted for by decay, indicating that other processes were affecting ³⁵S concentrations. The most likely explanation is that exchange with sediments or the biota was removing ³⁵S from the lake and replacing it with older sulphate devoid of ³⁵S. In September of 1995 and 1996, ³⁵S concentrations increased, suggesting that atmospheric deposition is important in the sulphate flux of these lakes in late summer. Sulphur-35 concentrations in the spring water were highly variable but never higher than 3.6 mBq L^-1 and averaged 2 mBq L^-1. Using a simple mixing model, it was estimated that 75% of the spring water was derived from precipitation of previous years.     

Mineral, chemical and radiological investigation of a black sand at Touzla Cape, near Thessaloniki, Greece

A black-sand formation located at Touzla Cape, near Thessaloniki city, Greece, was investigated using optical microscopy, powder-XRD, SEM-EDS, INAA and in-situ -ray spectrometry. This black sand is mainly composed of ilmenite, magnetite, garnet, zircon and rutile. Also present, in minor or trace amounts, are quartz, sphene, pyroxenes, sillimanite, feldspars, biotite, haematite, tourmaline, chromite, niobian-rutile and pyrrhotite. Niobian-rutile and pyrrhotite were found as inclusions in ilmenite and magnetite respectively. The radioactivity measurements indicated contributions of the uranium and thorium radioactive series and of 40K and 137Cs, and the maximum value of the total absorbed dose rate in air was found to be 62, 172, 8 and 2 nGy h-1 respectively. The main radioactivity of the uranium and thorium series is attributed to the fractions of zircon (304 µg Th g-1 and 157 µg U g-1), of ilmenite (89 µg Th g-1) and to a lesser extent to the fraction of garnet (5 µg Th g-1). The zircon fraction also contained 5076 µg Hf g-1. Some minerals and elements (Ti, Zr, Hf, Th, U) contained in the black sand could be of potential economic value. The high proportions of monomineralic grains along with the variations observed in mineral phases, in colour, in sphericity, in roundness, in grain size, in composition and in mineral inclusions, imply that the minerals and grains were subjected to several cycles of weathering and sedimentation, as well as being derived from multiple source rocks and areas.     

成都市大气降尘放射性水平分析

本文介绍了成都市大气降尘放射性水平的监测结果。发现降尘中除有少量天然核素外,还尚存有以往大气层核试验释放的裂变核素９０Ｓｒ和１３７Ｃｓ。平均年沉降量９０Ｓｒ为１０２Ｂｑ·ｍ－２·Ｙ－１,１３７Ｃｓ为１３１Ｂｑ·ｍ－２·Ｙ－１。由大气９０Ｓｒ和１３７Ｃｓ沉降所致公众辐射剂量为１６８μＳｒ·ａ－１,是限值的２‰。所以,降尘中放射性造成的辐射影响是很小的。     

两种垃圾焚烧炉灰渣的重金属成分与放射性检测

对8种重金属As、Hg、Mn、Cr、Cu、Cd、Co、Ni和Pb在两种垃圾焚烧炉灰渣中的浓度分布,浸出毒性及放射性进行检测.样品(炉渣和飞灰)分别取自北京(循环流化床焚烧炉CFBI)和深圳(炉排焚烧炉)两台不同燃烧方式的垃圾焚烧炉.研究表明,CFBI炉渣及飞灰中的重金属As、Mn、Cu、Cd、Co含量在炉渣中含量最低,中灰次之,飞灰中含量最高.重金属Hg在炉渣和飞灰中的含量相当,在中灰中的含量最低;Cr和Ni在炉渣中的含量也偏高,在中灰和飞灰中的含量相当Pb含量依中灰、炉渣和飞灰的顺序逐渐升高.浸出毒性检测结果显示,循环流化床垃圾焚烧后炉渣及飞灰中的重金属浸出毒性远低于国家标准1～2个量级,重金属总体排放量较低.炉排炉垃圾焚烧的炉渣及飞灰中的重金属含量却高很多,尤其是Cr、Pb、Cd和Cu.放射性检测结果表明,两种焚烧所产生的灰渣放射性均低于国家标准.在排放时无需作任何放射性方面的处理.最后,对焚烧灰渣的稳定化技术进行了讨论.