科学技术与工程
科學技術與工程
과학기술여공정
Science Technology and Engineering
2015年
29期
29-32,56
,共5页
祝武权%汤达祯%喻廷旭%汪雷
祝武權%湯達禎%喻廷旭%汪雷
축무권%탕체정%유정욱%왕뢰
BET比表面%相对压力%常数C%DFT模型
BET比錶麵%相對壓力%常數C%DFT模型
BET비표면%상대압력%상수C%DFT모형
BET specific surface%relative pressure%constant C%DFT model
基于多分子层吸附理论的BET模型是最成熟、最常用于比表面测试的计算方法,然而,针对页岩样品在液氮温度下的氮气吸附数据,选取0.05~0.30间的相对压力点(适用于中孔材料)进行BET比表面计算时,将出现回归曲线相关系数较差、常数C为负值(无物理意义)情况,这一问题往往被测试者忽视。通过页岩的二氧化碳吸附数据运用DFT模型,计算出页岩的微孔分布可知,页岩含有大量0.5~1.0 nm之间的微孔,页岩纳米级孔隙分布范围广的特点是出现上述问题的根本原因,即页岩并非孔径分布较窄的介孔材料。通过调整相对压力点的选取范围,在相对压力0.05~0.20下计算页岩比表面其相关系数能达到0.9999以上,且在Y轴上产生正截距,该相对压力范围更为合理,计算出的BET比表面更为可靠。
基于多分子層吸附理論的BET模型是最成熟、最常用于比錶麵測試的計算方法,然而,針對頁巖樣品在液氮溫度下的氮氣吸附數據,選取0.05~0.30間的相對壓力點(適用于中孔材料)進行BET比錶麵計算時,將齣現迴歸麯線相關繫數較差、常數C為負值(無物理意義)情況,這一問題往往被測試者忽視。通過頁巖的二氧化碳吸附數據運用DFT模型,計算齣頁巖的微孔分佈可知,頁巖含有大量0.5~1.0 nm之間的微孔,頁巖納米級孔隙分佈範圍廣的特點是齣現上述問題的根本原因,即頁巖併非孔徑分佈較窄的介孔材料。通過調整相對壓力點的選取範圍,在相對壓力0.05~0.20下計算頁巖比錶麵其相關繫數能達到0.9999以上,且在Y軸上產生正截距,該相對壓力範圍更為閤理,計算齣的BET比錶麵更為可靠。
기우다분자층흡부이론적BET모형시최성숙、최상용우비표면측시적계산방법,연이,침대혈암양품재액담온도하적담기흡부수거,선취0.05~0.30간적상대압력점(괄용우중공재료)진행BET비표면계산시,장출현회귀곡선상관계수교차、상수C위부치(무물리의의)정황,저일문제왕왕피측시자홀시。통과혈암적이양화탄흡부수거운용DFT모형,계산출혈암적미공분포가지,혈암함유대량0.5~1.0 nm지간적미공,혈암납미급공극분포범위엄적특점시출현상술문제적근본원인,즉혈암병비공경분포교착적개공재료。통과조정상대압력점적선취범위,재상대압력0.05~0.20하계산혈암비표면기상관계수능체도0.9999이상,차재Y축상산생정절거,해상대압력범위경위합리,계산출적BET비표면경위가고。
The theory of BET model which based on multi-molecular layer adsorption is the most commonly and mature method used for specific surface testing .For the nitrogen adsorption data of shale samples which at liquid nitrogen testing temperature , slectting the relative pressure from 0.05 to 0.30 between ( indicated for mesoporous materials) the BET specific surface of the sample can be calculated , but it will appear the problem of poor correla-tion coefficient and negative constant C which is not allowed to happen , the problem is often subject to ignore .The micropore pore size distribution calculated by carbon dioxide adsorption data using the DFT model shows shales con -tain a mount of microporous which aperture between 0.5 ~1.0 nm.The characteristics of shales nanometer pore distribution is the fundamental reason for the emergence of above problems .In other words , shale is not the meso-porous materials and narrower pore size distribution .On the contrary , by selecting the relative pressure which from 0.05 to 0.20 calculating the specific surface , the correlation coefficient reached more than 0.999 9, and emerged positive intercept on the Y axis, the relative pressure range is more reasonable , and the calculated BET specific sur-face is more reliable .