原子能科学技术
原子能科學技術
원자능과학기술
ATOMIC ENERGY SCIENCE AND TECHNOLOGY
2014年
9期
1725-1728
,共4页
李咏梅%谭凯旋%周泉宇%刘泽华%李春光%周新尧
李詠梅%譚凱鏇%週泉宇%劉澤華%李春光%週新堯
리영매%담개선%주천우%류택화%리춘광%주신요
铀尾矿%氡析出率%蒙特卡罗模拟
鈾尾礦%氡析齣率%矇特卡囉模擬
유미광%동석출솔%몽특잡라모의
uranium tailings%radon exhalation rate%Monte-Carlo simulation
基于核反冲理论建立了铀尾矿氡析出的数学模型和蒙特卡罗模拟方法,模拟了不同含水饱和度条件下铀尾矿颗粒粒度对氡析出的影响。结果表明,镭分布于颗粒表面时,4种含水饱和度(5%、20%、50%、75%)条件下的 K均随颗粒尺寸的增大先增大后趋于稳定。镭分布在距颗粒表面34 nm和68 nm时,含水饱和度为5%或20%的条件下,K先增加后趋于稳定,而含水饱和度为50%或75%的条件下, K随颗粒尺寸的增大先稍有下降然后逐渐稳定。运用蒙特卡罗方法计算了各铀尾矿样品的氡析出率,计算的氡析出率与实测铀尾矿氡析出率符合较好,相对误差为3%~9%。
基于覈反遲理論建立瞭鈾尾礦氡析齣的數學模型和矇特卡囉模擬方法,模擬瞭不同含水飽和度條件下鈾尾礦顆粒粒度對氡析齣的影響。結果錶明,鐳分佈于顆粒錶麵時,4種含水飽和度(5%、20%、50%、75%)條件下的 K均隨顆粒呎吋的增大先增大後趨于穩定。鐳分佈在距顆粒錶麵34 nm和68 nm時,含水飽和度為5%或20%的條件下,K先增加後趨于穩定,而含水飽和度為50%或75%的條件下, K隨顆粒呎吋的增大先稍有下降然後逐漸穩定。運用矇特卡囉方法計算瞭各鈾尾礦樣品的氡析齣率,計算的氡析齣率與實測鈾尾礦氡析齣率符閤較好,相對誤差為3%~9%。
기우핵반충이론건립료유미광동석출적수학모형화몽특잡라모의방법,모의료불동함수포화도조건하유미광과립립도대동석출적영향。결과표명,뢰분포우과립표면시,4충함수포화도(5%、20%、50%、75%)조건하적 K균수과립척촌적증대선증대후추우은정。뢰분포재거과립표면34 nm화68 nm시,함수포화도위5%혹20%적조건하,K선증가후추우은정,이함수포화도위50%혹75%적조건하, K수과립척촌적증대선초유하강연후축점은정。운용몽특잡라방법계산료각유미광양품적동석출솔,계산적동석출솔여실측유미광동석출솔부합교호,상대오차위3%~9%。
A mathematical model and Monte-Carlo simulation method of radon exhala-tion from uranium tailings were developed based on the nuclear recoil theory .The grain size effect on radon exhalation under different moisture contents was simulated .When radium is distributed on grain surface , K increases with grain size and then remains a constant value under moisture contents of 5% ,20% ,50% and 75% .When radium is distributed to a depth of 34 nm or 68 nm from the surface ,K firstly increases with grain size and then reaches a constant value under moisture contents of 5% and 20% ,and K decreases with the increase of grain size and then becomes a constant value under mois-ture contents of 50% and 75% .The radon exhalation rate of the uranium tailings sam-ples was calculated by Monte-Carlo method .The calculated radon exhalation rate agrees well with that obtained by experiment ,and the relative error is 3%-9% .