CAJ | 학술논문

中国黄土的粒度分布由分布峰度较高、分选较好的粗粒组分和分布峰度较低、分选较差的细粒组分叠加组成；前者代表了冬季风盛行季节近距离低空搬运的粉尘物质，其粒度指示了东亚冬季风所主导的近地面气流的强度，它在全样中的含量可能反映了冬季风粉尘的沉积通量；细粒组分可能主要为常态存在的、由高空气流搬运的远源粉尘，代表了黄土高原原始粉尘的本底，它的粒度特征与北太平洋西风带粉尘基本一致，可能指示了主要由西风带控制的高空气流的强度。黄土的粒度分布函数可用代表这两个组分分布的两个WEIBULL函数的和函数表示。用实测粒度分布数据对分布函数进行拟合可计算出该分布函数的各参数，同时可获得黄土粒度的两个组分各自的分布函数及两个组分在总样中所占的百分比。
중국황토적립도분포유분포봉도교고、분선교호적조립조분화분포봉도교저、분선교차적세립조분첩가조성；전자대표료동계풍성행계절근거리저공반운적분진물질，기립도지시료동아동계풍소주도적근지면기류적강도，타재전양중적함량가능반영료동계풍분진적침적통량；세립조분가능주요위상태존재적、유고공기류반운적원원분진，대표료황토고원원시분진적본저，타적립도특정여북태평양서풍대분진기본일치，가능지시료주요유서풍대공제적고공기류적강도。황토적립도분포함수가용대표저량개조분분포적량개WEIBULL함수적화함수표시。용실측립도분포수거대분포함수진행의합가계산출해분포함수적각삼수，동시가획득황토립도적량개조분각자적분포함수급량개조분재총양중소점적백분비。
Grain - size distribution of Chinese loess consistently shows bimode spectrum, which is composed of two dis-tinct components. The main component is coarse grain size with, large kurtosis and narrow distribution range,makes up main part of loess material. This main component is likely produced in the season when winter monsoondominate the paleoclimate of loess plateau, and therefore its grain size indicates East Asia winter monsoonstrength. The other grain size component has a wide distribution range, lower kurtosis and fine average grain size.This fine component probably represents the general dust base level of atmosphere over loess plateau, which pre-vails in most of the season. In some extension, it is genetically connected to the Northern Hemisphere westerly.Grain size distribution function of Chinese loess can be expressed with a sum of two Weibull distribution functionsthat represent two components of loess grain size. By fitting measured grain - size data to proposed distributionfunction, all parameters of the function can be estimated. Meanwhile, distribution function as well as the ratio ofthe two components can also be obtained.