爆炸与冲击
爆炸與遲擊
폭작여충격
EXPLOSION AND SHOCK WAVES
2009年
5期
486-491
,共6页
唐玉志%马远良%蔡宗义%吴祖堂%王占江
唐玉誌%馬遠良%蔡宗義%吳祖堂%王佔江
당옥지%마원량%채종의%오조당%왕점강
爆炸力学%关联响应模型%脉冲响应%化学爆炸%应力波
爆炸力學%關聯響應模型%脈遲響應%化學爆炸%應力波
폭작역학%관련향응모형%맥충향응%화학폭작%응력파
mechanics of explosion%relevant response model%impulse response%chemical explosion%stress wave
分析了弹性区域中应力传播的波动方程,说明该应力传播过程可以使用线性系统模型进行描述.根据系统辨识领域的脉冲响应方法,建立了应力测点的脉冲序列与源函数和响应序列之间的关系.在此基础上,建立了各测点间应力序列之间的关联响应模型,给出了采用神经网络的自适应优化方法求解关联参数的方法,并采用某次黄土介质中化学爆炸的实验数据进行了验证.将该模型用于测点数据的预测,预测值和实测值之间的误差很小.这表明,各测点间存在与测量数据无关的客观联系,仅由实验中爆炸源、测点位置和地介质力学参数分布等所决定.
分析瞭彈性區域中應力傳播的波動方程,說明該應力傳播過程可以使用線性繫統模型進行描述.根據繫統辨識領域的脈遲響應方法,建立瞭應力測點的脈遲序列與源函數和響應序列之間的關繫.在此基礎上,建立瞭各測點間應力序列之間的關聯響應模型,給齣瞭採用神經網絡的自適應優化方法求解關聯參數的方法,併採用某次黃土介質中化學爆炸的實驗數據進行瞭驗證.將該模型用于測點數據的預測,預測值和實測值之間的誤差很小.這錶明,各測點間存在與測量數據無關的客觀聯繫,僅由實驗中爆炸源、測點位置和地介質力學參數分佈等所決定.
분석료탄성구역중응력전파적파동방정,설명해응력전파과정가이사용선성계통모형진행묘술.근거계통변식영역적맥충향응방법,건립료응력측점적맥충서렬여원함수화향응서렬지간적관계.재차기출상,건립료각측점간응력서렬지간적관련향응모형,급출료채용신경망락적자괄응우화방법구해관련삼수적방법,병채용모차황토개질중화학폭작적실험수거진행료험증.장해모형용우측점수거적예측,예측치화실측치지간적오차흔소.저표명,각측점간존재여측량수거무관적객관련계,부유실험중폭작원、측점위치화지개질역학삼수분포등소결정.
Equations of motion were analyzed for governing underground explosion-induced stress waves spreading in an elastic domain to explain that this stress wave transmission processes could be described by a time-independent linear system model. According to the impulse response methods in the system identification field, the relationships were established to link the impulse series and source functions in the measured points with the response series. Based on the established relationships, a response model was developed to depict the relevancy between the stress series in the measured points. And a method was introduced to calculate the relevant parameters by adopting the adaptive optimization method of neural network and some important parameters were listed. The relevant response model was validated by the experimental data for a certain chemical explosion in soil. The predictions by the relevant response model are in agreement with the measured data and the relevancy between different measured points is determined only by the distributions of the explosion source, measured points and geological parameters.