从月亮的采样地点(总计的 46sampling 地点) 的 Clementine UVVIS 和 NIR 数据被处理并且过去常精制 Le Moueic 等的铁决心方法(2000, 2002 ) 。我们发现大约 21 个采样地点是对 Le Moueic 等不合适“ s 光谱参数(”斜坡“并且”深度 1'') 因为他们的 1500 nm 过滤器不能被用作光谱参数“右肩膀并且评估 1-μ m 的深度吸收特征精确地。Weused 精制方法的 25 个采样地点由 Le Moueic 等开发了的剩余的。(2000, 2002 ) 并且获得了我们 FeO 内容决心的自己的方程。我们测试了我们的自己的方程,和结果是 satifactory。在我们的工作,我们也在我们 Chang 的自己的数据集的科学应用程序获得了一些有用经验“ E-1 使命。
Clementine UVVIS and NIR data from the lunar sampling sites (totaling 46 sampling sites) were processed and used to refine the iron determination method of Le Mou6ic et al. (2000, 2002). We found that about 21 sampling sites are unsuitable to Le Mou6ic et al's spectral parameters ("slope" and "depth 1") because their 1500 nm filter could not be used as spectral parameters' right shoulders and to evaluate the depth of the 1-1am absorption feature accurately. We used the rest 25 sampling sites to refine the method developed by Le Mou6ic et al. (2000, 2002 ) and obtained our own equation of FeO content determination. We tested our own equation, and the results are satifactory. In our work we also acquired some useful experiences in scientific applications of our own dataset of the Chang 'E- 1 mission.