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数字化γ能谱测井探管研制

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针对铀钍混合型矿床上无法精确测量地层中铀、钍含量的问题,本文研制了一台基于溴化铈晶体的数字化γ能谱测井探管.该仪器采用直径 38 mm×38 mm的溴化铈晶体,提高了铀灵敏度和在低铀、低钍含量矿层的探测效率.采用C8051 单片机作为核心处理器,对溴化铈探测器原始信号进行了滤波成形处理,通过能谱采集器得到γ能谱数据.通过对γ能谱数据进行逆矩阵解谱,即可得到矿层中铀、钍的精确含量.通过RS-485 总线将γ能谱数据传送至测井主机.测试结果表明:本仪器在标准铀钍混合模型上的测量准确度高,其示值误差小于 6%,稳定性小于 1.5%,重复性小于1%,钍系208 Tl的2.62 MeV能量峰漂移不超过±0.3 道,检查测井异常相对误差小于4%,可应用于铀矿勘查测井工作.
Development of a digital γ spectral logging probe
Given that it is difficult to accurately determine the uranium and thorium contents in the strata of uranium-thorium mixed de-posits,this study developed a digital γ spectrum logging probe based on cerium tribromide(CeBr3)crystals.Using CeBr3 crystals with a diameter of 38 mm×38 mm,the logging probe improved the sensitivity to uranium and the detection efficiency of ore beds with low u-ranium and thorium contents.The logging probe operated as follows.First,the original signals from the CeBr3 detector were filtered and shaped using the C8051 single-chip microcomputer as the core processor.Then,the γ spectrum data were obtained using the energy spectrum collector.After the spectrum unfolding based on the inverse matrix is performed for the γ spectrum data,precise uranium and thorium contents in the ore beds were obtained.Finally,the γ spectrum data were transmitted to the host computer for logging through the RS-485 bus.The results show that the logging probe had high measurement accuracy in the standard uranium-thorium mixed model,with indication errors of less than 6%,stability of less than 1.5%,and repeatability of less than 1%.Moreover,the 2.62 MeV energy peak drift of thorium 208 Tl did not exceed±0.3 channels,and the relative errors of log anomalies were less than 4%.Therefore,the digit-al γ spectrum logging probe proposed in this study is applicable to the exploration and logging of uranium deposits.

γ spectral logcerium bromidespectrum unfolding based on the inverse matrix

陈元庆、黄清波、刘金尧、王先贺、黄亮、吴伟军

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核工业航测遥感中心,河北 石家庄 050011

γ能谱测井 溴化铈 逆矩阵解谱

中核集团集中研发

物SD03-01

2024

物探与化探
中国国土资源航空物探遥感中心

物探与化探

CSTPCD
影响因子:0.828
ISSN:1000-8918
年,卷(期):2024.48(1)
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