Coal mining can dramatically change hydrogeological conditions and induce serious environmental problems. Fifty groundwater samples were collected from the main aquifers in the Yuaner coal mine (Anhui Province, China). The results show that the main hydrogeochemical processes in the mine include dissolution, precipitation, pyrite oxidation, desulfurization, and cation exchange. The Neogene porous aquifer is affected by groundwater flow conditions; its main hydrogeochemical processes are dissolution of carbonate minerals and gypsum, and cation exchange. The Permian coal measure’s fractured sandstone aquifer was confirmed to be controlled by the region’s geological structure; its main hydrogeochemical processes are desulfurization and cation exchange. The Carboniferous Taiyuan limestone aquifer was determined by both groundwater flow conditions and regional geological structure; its main hydrogeochemical processes are dissolution of carbonate minerals and gypsum, pyrite oxidation, and cation exchange. Additionally, hydrogeochemical inverse modeling of the groundwater flow path confirm the hydrochemistry results and principal component analysis.
酸土脂环酸芽孢杆菌(Alicyclobacillus acidoterrestris)是引起橙汁劣变的主要微生物,为研究酸土脂环酸芽孢杆菌在橙汁中的生长规律,利用近红外光谱获取橙汁中酸土脂环酸芽孢杆菌含量的信息,采用标准化(autoscale)、多元散射校正(multiplicative scatter correction,MSC)、标准正态变换(standard normal variate,SNV)、去趋势化(detrend)对光谱进行预处理,结合化学计量学,构建近红外光谱与酸土脂环酸芽孢杆菌含量预测模型。在此基础上,将近红外光谱转换为酸土脂环酸芽孢杆菌预测菌落数据,并采用“一步法”直接基于预测菌落数构建橙汁中酸土脂环酸芽孢杆菌的生长模型。结果表明,利用标准化进行光谱预处理建立的偏最小二乘(partial least squares,PLS)模型对橙汁中酸土脂环酸芽孢杆菌含量的预测效果相对较好,其预测决定系数(prediction determination coefficient,Rp2)与预测均方根误差(root mean square error of prediction... 相似文献