岩矿测试
巖礦測試
암광측시
ROCK AND MINERAL ANALYSIS
2009年
4期
388-390
,共3页
杨理勤%冯亮%李玄辉%陈占生
楊理勤%馮亮%李玄輝%陳佔生
양리근%풍량%리현휘%진점생
高含量金%哈测金-1%均匀性
高含量金%哈測金-1%均勻性
고함량금%합측금-1%균균성
high-content of gold%HACEAu-1%homogeneity
利用王水溶样,残渣经氢氟酸、高氯酸分解-活性炭吸附-原子吸收光谱法测定了高含量金样品"哈测金-1"的15个子样中的全金量,并对子样进行了平行双份分析.考察了天平称量精度、玻璃器皿刻度精度和活性炭吸附率造成的测量不确定度,并估算出合成不确定度范围为2.5%~4.2%;论证了方法的可行性.对单个子样重复分析结果的可靠性及其算术平均值的极限误差进行了评估,计算出样品均匀性质量参数为0.70,依此判定该样品的均匀性质量等级为"良好".
利用王水溶樣,殘渣經氫氟痠、高氯痠分解-活性炭吸附-原子吸收光譜法測定瞭高含量金樣品"哈測金-1"的15箇子樣中的全金量,併對子樣進行瞭平行雙份分析.攷察瞭天平稱量精度、玻璃器皿刻度精度和活性炭吸附率造成的測量不確定度,併估算齣閤成不確定度範圍為2.5%~4.2%;論證瞭方法的可行性.對單箇子樣重複分析結果的可靠性及其算術平均值的極限誤差進行瞭評估,計算齣樣品均勻性質量參數為0.70,依此判定該樣品的均勻性質量等級為"良好".
이용왕수용양,잔사경경불산、고록산분해-활성탄흡부-원자흡수광보법측정료고함량금양품"합측금-1"적15개자양중적전금량,병대자양진행료평행쌍빈분석.고찰료천평칭량정도、파리기명각도정도화활성탄흡부솔조성적측량불학정도,병고산출합성불학정도범위위2.5%~4.2%;론증료방법적가행성.대단개자양중복분석결과적가고성급기산술평균치적겁한오차진행료평고,계산출양품균균성질량삼수위0.70,의차판정해양품적균균성질량등급위"량호".
15 samples, named "HACEAu-1", with high-content of gold were digested with aqua regia and the residues were decomposed with HF-HClO4. Gold in the sample solution was preconcentratcd by activated carbon adsorption and determined by FAAS. Duplicate analysis for 15 samples was carried out and the measurement uncertainty for the analytical results was evaluated. The main sources of measurement uncertainty came from sub-uncertainties of the analytical balance, scale accuracy of the analytical glassware, gold adsorption rate by activated carbon. The composed uncertainty was calculated with a range of 2.5% to 4.2%, which means that the method was feasible. The reliability for the results from duplicate analysis of single sample and the limiting error of its arithmetic mean value were also evaluated. The homogeneity quality coefficient of the sample was calculated as 0.70, which means that the sample was in "good" homogeneity quality grade.