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FALLOUT OF URANIUM AND PLUTONIUM FROM RECENT VOLCANIC ERUPTIONS (ARKANSAS).

机译:近期火山喷发(铀矿)中铀和P的沉降。

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摘要

The concentrations of ('234)U, ('235)U, ('238)U in rain water were measured in a total of 102 individual samples which were collected at Fayetteville, Arkansas, from July 1980 through April 1983. A spectacular increase in the heavy isotope of uranium (('238)U) was observed in the months of July, August (1980); January through April, November and December 1981. This large increase in ('238)U in rain appeared to have had its origin in the May 1980 eruption of Mount St. Helens. An increase in the concentration of ('238)U in rain, smaller than 1981, was observed, which seems to have originated from the "El Chichon" volcano eruption in March 1982, and the spring peak or so-called cycling effect. The excess deposition of ('238)U brought down by the rain and snow at Fayetteville, Arkansas, from March 1980 through December 1982, was found to be 3.13 fCi/cm('2).;The concentrations of ('238,239,240)Pu were measured in 101 individual rain samples which were collected at Fayetteville, Arkansas, during the period from January 1981 through April 1983. A striking increase in the average bimonthly concentration of ('239,240)Pu occurred during the months of September-October 1980 (15.6 fCi/l) and March-April 1981 (29.4 fCi/l). The increase in the ('239,240)Pu concentration in rain occurred just about the time the fission products (('89,90)Sr) from the 25th Chinese nuclear test appeared at Fayetteville, Arkansas. The excess deposition of ('239,240)Pu brought down by the rain at Fayetteville, Arkansas, from March 1980 through December 1982 was found to be 1.01 fCi/cm('2). The total amount of ('239,240)Pu deposited at Fayetteville, Arkansas, from March through December 1982, was found to be about 30 times higher than the total amount calculated from reported literature values. The excess ('239,240)Pu has been attributed to stratospheric ('239,240)Pu from nuclear weapons testing prior to the 25th Chinese nuclear test. Also, the spring peak effect on ('238)Pu, ('239,240)Pu in rain suggested by Rao (1978) was confirmed.
机译:从1980年7月至1983年4月在阿肯色州费耶特维尔收集的总共102个单独样品中测量了雨水中的('234)U,('235)U,('238)U浓度。在1980年7月,8月的几个月中观察到铀(('238)U)的重同位素; 1981年1月到4月,11月和12月。雨中('238)U的大量增加似乎起源于1980年5月的圣海伦斯火山喷发。观察到在雨中('238)U的浓度增加,小于1981年,这似乎是由于1982年3月的“ El Chichon”火山喷发以及春季高峰或所谓的循环效应引起的。从1980年3月至1982年12月,阿肯色州费耶特维尔的雨雪造成的('238)U过量沉积为3.13 fCi / cm('2)。;('238,239,240)Pu的浓度在1981年1月至1983年4月期间从阿肯色州Fayetteville收集的101个降雨样本中进行了测量。1980年9月至10月的两个月中,Pu的平均双月浓度显着增加('239,240)(15.6 fCi / l)和1981年3月-4月(29.4 fCi / l)。雨中('239,240)Pu浓度的增加恰好来自第25次中国核试验的裂变产物(('89,90)Sr)出现在阿肯色州的费耶特维尔。从1980年3月到1982年12月,由于降雨在阿肯色州费耶特维尔造成的('239,240)Pu过量沉积为1.01 fCi / cm('2)。从1982年3月至1982年12月,在阿肯色州Fayetteville沉积的('239,240)Pu总量比根据报告的文献值计算的总量高约30倍。多余的('239,240)Pu归因于第25次中国核试验之前进行的核武器试验所产生的平流层('239,240)Pu。另外,证实了Rao(1978)提出的春季峰值对('238)Pu,('239,240)Pu的春季影响。

著录项

  • 作者

    SANDOVAL, DEIG-NEVY.;

  • 作者单位

    University of Arkansas.;

  • 授予单位 University of Arkansas.;
  • 学科 Chemistry Nuclear.
  • 学位 Ph.D.
  • 年度 1984
  • 页码 131 p.
  • 总页数 131
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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