1) quantitative change accumulation
量变积累
1.
Discussion on the mode and conditions of quantitative change accumulation in conflict transform;
论矛盾转化中量变积累的形式与条件
2) cumulant variable
累积变量
1.
The method of removing statistics fluctuation with factorial moment was introduce and the cumulant variable able to even for distribution of multiparticle production was proved.
本文介绍了用阶乘矩能够消除统计起伏，证明引入累积变量后可使粒子数的分布变得均匀；给出了消除粒子间关联效应的方
3) cumulate deformation
累积变形量
1.
Wheel-rutting index(WRI),a new index for evaluating the whole-term high-temperature stability of asphalt mixture is presented by taking into account all the factors affecting the high-temperature performance,such as the velocity,the cumulate deformation and the maximal permanent deformation,and the analysis and comparison of the degrees of track ruts in different periods are then carried out.
提出了车辙系数(WR I)指标这一概念,综合考虑了行车速率、累积变形量和最大永久变形量等因素对压实沥青混合料高温性能的影响,对不同时间车辙发生的程度进行了对比、分析。
4) time-varying cumulants
时变累积量
5) accumulative deformation
累积变形
1.
Research on accumulative deformation behavior of soft clay under cyclic loads;
循环荷载作用下软粘土的累积变形特性的研究
2.
Compared with other kinds of sensors,module matching FBG has a better test effect,and this kind of FBG is able to reflect the accumulative deformation of asphalt mixture to some extent.
结果表明,采用应变修正后的光纤光栅应变传感器进行路面结构内部应变实测是可行的;模量匹配光纤光栅应变传感器与其它类型传感器相比具有较好的测试效果,同时该类型传感器在一定程度上能够反映出沥青混合料的累积变形。
6) strain accumulation
应变积累
1.
By use of horizontal velocity data observed by GPS during 2001—2004 and 2004—2007 in the northeastern margin of Qinghai-Tibet block,aided by the negative dislocation model,the characteristics of horizontal crustal movement and the status of strain accumulation of this area are researched and following conclusion are drawn.
利用青藏块体东北缘2001—2004年、2004—2007年GPS水平运动速度场结果,借助负位错模型,研究该区当前的地壳水平运动特征与应变积累状况。
2.
By use of the regional leveling and GPS observations in Sichuan-Yunnan area during 1994-2006,aided by the negative dislocation model for the elastic block boundaries,combining with the total characteristics of deformation cross-fault,the recent status and intensity of strain accumulation of tectonic blocks and their boundary faults in Sichuan-Yunnan area are studied.
利用1994～2006年川滇地区GPS和区域水准观测资料,借助弹性块体边界负位错模型,结合近年来跨断层形变总体特征,研究了川滇地区构造块体及其边界断裂的应变积累状况与强度。
补充资料：降水量变率
降水量变率
precipitation variability
区，变率愈小;降水量愈小的地区，变率愈大。长江以南、西南地区·般为1《跳~15%;东南沿海地区因受台风影响，变率较大，为15%~2哎踢;华北大部分地区大于25%;河北省中部和河套·带可达艾践左右、东北大部分地区为生O%~巧%;西北和内蒙古高原在义准以L，塔里木盆地可达父肠。4~6月降水量变率:黄淮海平原多在粼洲以上;江南和华南多在20系左右，沿海约为艾既;西南地区在2口荡以卜。7~8月降水量变率:华北平原达30%~粼现，;江南高达闷仓笼以上;华南在卫冷以上;东北地区在3心叉场以下。(朱淑兰)1 iangshuiliang bianIO降水t变率(p，initation variability)表示某一地点降水量平均偏差相对于平均值的变化程度。一般分为绝对变率和相对变率。绝对变率是降水量序列中各要素距平绝对值的算术平均值，其表达式为: 才__l<--，:，二. 几‘二1式中d为绝对变率;;‘为降水量序列中的第i个要素值(i=l，2，……，n);n为样本数;不为序列平均值。相对变率V是绝对变率占平均降水量的百分率，即 F二婆、1哪 r降水变率小，表示年际间变化小，降水量比较稳定;反之，变率大，表示年际间变化大，偏旱年、多雨年的可能性大，易发生早涝。中国各地年降水量变率分布总的特点是:降水量愈大的地
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条