Nội dung được dịch bởi AI, chỉ mang tính chất tham khảo
Tác động của sự phân bố các mặt khoáng phản ứng đến tính chất hấp thụ radionuclide trong các loại đá granite không đồng nhất đa quy mô
Tóm tắt
Việc mô hình hóa sự vận chuyển phản ứng của radionuclide trong các đá chủ là một trong những thách thức lớn nhất đối với việc đánh giá hiệu suất và an toàn của các kho chứa rác thải phóng xạ mức cao. Tính không đồng nhất của đá có ảnh hưởng đáng kể đến các ảnh hưởng quy mô của các thông số dòng chảy và vận chuyển chất hòa tan như hệ số hấp thụ. Việc quy mô hóa hệ số hấp thụ radionuclide liên quan đến sự phân bố của các mặt khoáng phản ứng (RMF) trong các đá nứt, có thể được mô phỏng bằng các phương pháp địa thống kê dựa trên xác suất chuyển tiếp. Các phân tích địa thống kê và hóa địa hóa học của sự phân bố RMF được thực hiện trên các mẫu granite lấy từ địa điểm Beishan ở tây bắc Trung Quốc. Bài báo này trình bày một phương pháp để xác định RMF bằng cách sử dụng mô hình nhận dạng khoáng sản dựa trên học sâu. Tỷ lệ thể tích và chiều dài trung bình của RMF được ước lượng một cách chính xác theo cách này so với kết quả phân tích nhiễu xạ X-ray. Phương pháp này khắc phục được những hạn chế của các phương pháp truyền thống vốn mang tính chất chủ quan và có độ chính xác thấp hơn. Kết quả cho thấy mô hình hiệp phương sai tổng hợp của các hệ số hấp thụ liên quan đến tỷ lệ thể tích và chiều dài trung bình của RMF. Hệ số hấp thụ hiệu quả được thu được bằng mô hình quy mô lớn lớn hơn trung bình hình học và nhỏ hơn trung bình số học. Hơn nữa, thông qua phân tích độ nhạy toàn cầu, người ta phát hiện rằng các yếu tố làm chậm trung bình có tác động lớn nhất đến hệ số hấp thụ hiệu quả. Kết quả của nghiên cứu này cung cấp thông tin quan trọng để nâng cao hiểu biết về quá trình vận chuyển radionuclide trong granite nứt.
Từ khóa
#radionuclide #hấp thụ #mặt khoáng phản ứng #granite không đồng nhất #mô hình học sâuTài liệu tham khảo
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