对陕西岐山县礼村的周原黄土进行了磁化率和穆斯堡尔谱的测试，样品选自礼村黄土剖面中的马兰黄土、褐红色顶层埋藏土、褐色顶层埋藏土和新近黄土各个层位，它们是在不同的气候条件下形成的。根据对样品穆斯堡尔谱的测试，可以得到黄土全样和非磁分裂组分中Ｆｅ￣（３＋）／Ｆｅ￣（２＋）＋Ｆｅ￣（３＋）、全样中全铁的相对含量以及全样、磁分裂组分和非磁分裂组分中Ｆｅ￣（３＋）的相对含量。结果表明，磁化率与上述由穆斯堡尔谱学可法所得到的各个量之间都存在着较好的线性关系，并根据形成这些黄土的气候条件定性地解释了这些线性关系的存在。 Magnetic susceptibility and Mossbauer spectroscopy were tested on Zhouyuan loess in Li village of Shaanxi Province. The samples were selected from Malan loess, maroon top buried soil, brown top buried soil and recent loess layers Bit, they are formed under different climatic conditions. Based on the Mossbauer spectroscopy of the samples, the relative contents of Fe ~ (3 +) / Fe ~ (2+) + Fe ~ (3+) The relative content of Fe ~ (3 +) in both magnetic and non-magnetic components. The results show that there is a good linear relationship between the magnetic susceptibility and the quantities obtained by the above Mossbauer spectroscopy, and the existence of these linear relationships is qualitatively explained according to the climatic conditions for forming these loess.