伊犁师范学院学报(自然科学版)
伊犛師範學院學報(自然科學版)
이리사범학원학보(자연과학판)
JOURNAL OF ILI NORMAL UNIVERSITY
2013年
4期
29-33
,共5页
张丽英%张晓媛%张丽丽%李玉强%黄以能
張麗英%張曉媛%張麗麗%李玉彊%黃以能
장려영%장효원%장려려%리옥강%황이능
水泥%水化反应%显微图像
水泥%水化反應%顯微圖像
수니%수화반응%현미도상
cement%hydration reaction%microscopic image
用光学显微镜和电子天平相结合的方法,在室温(约290K)、1个大气压、相对湿度约45%的条件下,对水泥浆体的显微图像和质量进行了实时的测量.结果表明,水泥的水化反应可以划分为4个过程:1)0至t1(=8.3min)的I过程,水泥浆体的约化亮度I s随t近似线性增加,同时约化质量m随t线性减小;2) t1至t2(=27.9min)的II过程,Is随t快速近似线性增加,同时m随t线性减小;3)t2至t3(=46.3min)的III过程,随时间t的增加,m先快速、然后缓慢下降到稳定值, Is几乎不变;4)t3以后的VI过程,m和Is不随t变化.水泥浆体质量减少是因为其中水的挥发,其颜色变淡是因为其中CH的形成. t1之前CH的形成率较低,而t1至t2是CH形成率较快的时期, t2之后已经基本没有CH形成.因此, t1、t2分别表征的是诱导期、加速期的结束.从t2至t3时期,浆体中水仍有少量挥发,但已经不再有CH的生成. t3以后,浆体水分挥发得极少,也不再有CH的生成.
用光學顯微鏡和電子天平相結閤的方法,在室溫(約290K)、1箇大氣壓、相對濕度約45%的條件下,對水泥漿體的顯微圖像和質量進行瞭實時的測量.結果錶明,水泥的水化反應可以劃分為4箇過程:1)0至t1(=8.3min)的I過程,水泥漿體的約化亮度I s隨t近似線性增加,同時約化質量m隨t線性減小;2) t1至t2(=27.9min)的II過程,Is隨t快速近似線性增加,同時m隨t線性減小;3)t2至t3(=46.3min)的III過程,隨時間t的增加,m先快速、然後緩慢下降到穩定值, Is幾乎不變;4)t3以後的VI過程,m和Is不隨t變化.水泥漿體質量減少是因為其中水的揮髮,其顏色變淡是因為其中CH的形成. t1之前CH的形成率較低,而t1至t2是CH形成率較快的時期, t2之後已經基本沒有CH形成.因此, t1、t2分彆錶徵的是誘導期、加速期的結束.從t2至t3時期,漿體中水仍有少量揮髮,但已經不再有CH的生成. t3以後,漿體水分揮髮得極少,也不再有CH的生成.
용광학현미경화전자천평상결합적방법,재실온(약290K)、1개대기압、상대습도약45%적조건하,대수니장체적현미도상화질량진행료실시적측량.결과표명,수니적수화반응가이화분위4개과정:1)0지t1(=8.3min)적I과정,수니장체적약화량도I s수t근사선성증가,동시약화질량m수t선성감소;2) t1지t2(=27.9min)적II과정,Is수t쾌속근사선성증가,동시m수t선성감소;3)t2지t3(=46.3min)적III과정,수시간t적증가,m선쾌속、연후완만하강도은정치, Is궤호불변;4)t3이후적VI과정,m화Is불수t변화.수니장체질량감소시인위기중수적휘발,기안색변담시인위기중CH적형성. t1지전CH적형성솔교저,이t1지t2시CH형성솔교쾌적시기, t2지후이경기본몰유CH형성.인차, t1、t2분별표정적시유도기、가속기적결속.종t2지t3시기,장체중수잉유소량휘발,단이경불재유CH적생성. t3이후,장체수분휘발득겁소,야불재유CH적생성.
Integrating light microscope with electronic balance, the microscopic image and mass of the cement paste were measured in real-time under one bar pressure and 45%RH (relative humidity) at room temperature (about 290K). The result shows that hydration reactions of the cement can be divided into four processes: 1) process-I appears from 0 to t 1 (=8.3min) where the reduced luminance (I) of the cement pastes increases, while the reduced mass (m) decreases with time;2) process-II starts from t1 to t2 (=8.3min), and during which I goes up rapidly meanwhile m declines with time; 3) process-III emerges between t2 to t3 (=27.9min) where m drops first rapidly and then slowly to a steady value, but I almost keeps constant with time;4) process-IV arises after t3, and both I and m do not vary with time. Combining the knowledge about hydration reaction of cement with the author’s some new ideas, it was proposed that I originates from evaporation of the water, while the fading color results in the form of Ca(OH) 2 (CH). In the process-I, the formation of CH is at low rate, but the formation rate comes faster during the process-II, and there is no formation of CH after the process-II. So, t1 and t2 expresses, respectively, the end of the initial period and acceleration period. From t2 to t3, a little water of cement still volatilizes, but no CH generates. There is little water to volatilize and CH also does not form after t3.