Chemical Industry and Engineering Progress ›› 2025, Vol. 44 ›› Issue (9): 5391-5405.DOI: 10.16085/j.issn.1000-6613.2025-0121
• Resources and environmental engineering • Previous Articles
DUAN Xianzhe1,2(
), BI Wenting1, LI Nan2,3, DOU Jiale1, SHAO Bingqing1, WANG Jiawei1, WU Peng1, HUANG Huan1, TANG Zhenping1,2(
)
Received:2025-01-21
Revised:2025-04-13
Online:2025-09-30
Published:2025-09-25
Contact:
TANG Zhenping
段先哲1,2(
), 毕文婷1, 李南2,3, 豆佳乐1, 邵冰清1, 汪佳伟1, 吴鹏1, 黄欢1, 唐振平1,2(
)
通讯作者:
唐振平
作者简介:段先哲(1985—),男,博士,副教授,硕士生导师,研究方向为放射性废物处置。E-mail:duanxianzhe@usc.edu.cn。
基金资助:CLC Number:
DUAN Xianzhe, BI Wenting, LI Nan, DOU Jiale, SHAO Bingqing, WANG Jiawei, WU Peng, HUANG Huan, TANG Zhenping. Numerical simulation for disposal of high-level radioactive wastes (HLWs): Mechanisms and influencing factors of radionuclide migration[J]. Chemical Industry and Engineering Progress, 2025, 44(9): 5391-5405.
段先哲, 毕文婷, 李南, 豆佳乐, 邵冰清, 汪佳伟, 吴鹏, 黄欢, 唐振平. 数值模拟在高放废物处置中的应用:放射性核素迁移机制及其影响因素[J]. 化工进展, 2025, 44(9): 5391-5405.
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URL: https://hgjz.cip.com.cn/EN/10.16085/j.issn.1000-6613.2025-0121
| 基本原理 | 处置方法 | 基本思想 | 特点 | |
|---|---|---|---|---|
| 滞留-衰变 | 核嬗变法 | 将高放废物转变为低放废物 | 过程繁杂且耗能大,嬗变后仍然需要处置放射性废物 | |
| 浓缩-封隔 | 隔离法 | |||
| 宇宙隔离 | 将核废物送出地球以外的宇宙空间 | 花费大,受国际形势与技术条件的限制 | ||
| 海洋隔离 | 将高放废物容器置入深海底部黏土沉积物深处 | 违反国际法 | ||
| 岩石融化隔离 | 直接将高放废液注入钻孔或深部岩硐中 | 耗资巨大,技术复杂,目前只是设想 | ||
| 冰层隔离 | 将核废物球放入较为稳定的冰原 | 冰原会发生移动,违反国际法 | ||
| 深地质处置隔离 | 将核废物埋入地层深处 | 可行,且下一代有重新处置废物的选择 | ||
| 稀释-分散 | 稀释法 | 对核废物净化或衰减到排放标准以下再稀释扩散到环境中去 | 不能处置乏燃料产生的废物 | |
| 基本原理 | 处置方法 | 基本思想 | 特点 | |
|---|---|---|---|---|
| 滞留-衰变 | 核嬗变法 | 将高放废物转变为低放废物 | 过程繁杂且耗能大,嬗变后仍然需要处置放射性废物 | |
| 浓缩-封隔 | 隔离法 | |||
| 宇宙隔离 | 将核废物送出地球以外的宇宙空间 | 花费大,受国际形势与技术条件的限制 | ||
| 海洋隔离 | 将高放废物容器置入深海底部黏土沉积物深处 | 违反国际法 | ||
| 岩石融化隔离 | 直接将高放废液注入钻孔或深部岩硐中 | 耗资巨大,技术复杂,目前只是设想 | ||
| 冰层隔离 | 将核废物球放入较为稳定的冰原 | 冰原会发生移动,违反国际法 | ||
| 深地质处置隔离 | 将核废物埋入地层深处 | 可行,且下一代有重新处置废物的选择 | ||
| 稀释-分散 | 稀释法 | 对核废物净化或衰减到排放标准以下再稀释扩散到环境中去 | 不能处置乏燃料产生的废物 | |
| 类别 | 低放废物(LLWs) | 中放废物(ILWs) | 高放废物(HLWs) |
|---|---|---|---|
| 放射性水平 | 较低,无需屏蔽 | 中等,需要屏蔽 | 高,需要严格屏蔽并管理 |
| 主要来源 | 铀矿生产、核电站运行、防护用品、医疗废物、科研实验 | 核燃料前处理、乏燃料后处理、污染管道、冷却水沉积物 | 乏燃料、高活性废液、核武器试验 |
| 处理复杂度 | 简单,压缩、固化或浅层填埋 | 复杂,需固化及深地质处置 | 高度复杂,需玻璃固化和深地质处置 |
| 环境风险 | 低,规范管理下影响小 | 较高,若管理不当可能污染地下水 | 极高,管理不当可能造成严重环境和健康危害 |
| 体积比例 | 大,占大部分废物体积 | 较小 | 小,但活度极高 |
| 代表核素 | 86Rb、90Y | 90Sr、137Cs | 79Se、99Tc、237Np、239Pu、241Am |
| 类别 | 低放废物(LLWs) | 中放废物(ILWs) | 高放废物(HLWs) |
|---|---|---|---|
| 放射性水平 | 较低,无需屏蔽 | 中等,需要屏蔽 | 高,需要严格屏蔽并管理 |
| 主要来源 | 铀矿生产、核电站运行、防护用品、医疗废物、科研实验 | 核燃料前处理、乏燃料后处理、污染管道、冷却水沉积物 | 乏燃料、高活性废液、核武器试验 |
| 处理复杂度 | 简单,压缩、固化或浅层填埋 | 复杂,需固化及深地质处置 | 高度复杂,需玻璃固化和深地质处置 |
| 环境风险 | 低,规范管理下影响小 | 较高,若管理不当可能污染地下水 | 极高,管理不当可能造成严重环境和健康危害 |
| 体积比例 | 大,占大部分废物体积 | 较小 | 小,但活度极高 |
| 代表核素 | 86Rb、90Y | 90Sr、137Cs | 79Se、99Tc、237Np、239Pu、241Am |
| 主要模型 | 适用条件 | 优点 | 缺点 | 常用模拟软件 |
|---|---|---|---|---|
| 等效连续介质模型 | 大区域、裂隙发育程度较高 | 所需数据易于获取技术成熟、操作性强 | 求解精度低、无法细致描述裂隙介质的不连续性和各向异性 | Modflow、GMS、Porflow |
| 离散裂隙网络模型 | 小尺度、单裂隙 | 精度高、拟真性好 | 工作量大、耗时长 | Connectflow |
| 双重介质模型 | 岩块的渗透率远小于裂隙渗透率 | 计算和概念上要求更低反应渗流特征更全面 | 溶质交换项难以确定、适用范围有限、计算复杂 | Though2 |
| 等效-离散耦合模型 | 分区域使用:裂隙密度大时使用等效连续介质模型;裂隙密度小时采用离散裂隙网络模型 | 精度高、拟真性好 | 水量交换难以确定、耦合操作技术难、数学计算难 | Feflow、Hydrogeosphere |
| 主要模型 | 适用条件 | 优点 | 缺点 | 常用模拟软件 |
|---|---|---|---|---|
| 等效连续介质模型 | 大区域、裂隙发育程度较高 | 所需数据易于获取技术成熟、操作性强 | 求解精度低、无法细致描述裂隙介质的不连续性和各向异性 | Modflow、GMS、Porflow |
| 离散裂隙网络模型 | 小尺度、单裂隙 | 精度高、拟真性好 | 工作量大、耗时长 | Connectflow |
| 双重介质模型 | 岩块的渗透率远小于裂隙渗透率 | 计算和概念上要求更低反应渗流特征更全面 | 溶质交换项难以确定、适用范围有限、计算复杂 | Though2 |
| 等效-离散耦合模型 | 分区域使用:裂隙密度大时使用等效连续介质模型;裂隙密度小时采用离散裂隙网络模型 | 精度高、拟真性好 | 水量交换难以确定、耦合操作技术难、数学计算难 | Feflow、Hydrogeosphere |
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