干旱区泥炭样品加热过程中磁学特征的变化研究  

Magnetic properties during heating of the peat sediments in arid regions

作　　者：张俊辉[1,2] 夏敦胜[1,3] 张英[1] 张健[4] 许淑婧[1] 刘宇航[1] 

机构地区：[1]兰州大学西部环境与气候变化研究院,甘肃兰州730000 [2]宝鸡文理学院灾害监测与机理模拟 陕西重点实验室,陕西宝鸡721006 [3]中国科学院寒区旱区环境与工程研究所 沙漠与沙漠化重点实验室,甘肃兰州730000 [4]复旦大学历史地理研究中心,上海200433

出　　处：《干旱区地理》2012年第6期938-945,共8页Arid Land Geography

基　　金：国家自然科学基金(中国西北地区大气降尘磁学特征时空变化研究,项目编号41071125);国家重点基础研究发展规划项目(末次冰盛期以来我国气候环境变化与干旱区人类的影响与适应,项目编号2010CB950204)

摘　　要：利用采自干旱区高山～新疆阿尔泰山的表层泥炭样品,以K-T曲线为主,结合J-T曲线、磁滞参数以及XRD等相关实验,探讨了应用热磁实验鉴别富含有机质的弱磁性物质磁性特征。结果表明:样品中磁化率的主要贡献者为低矫顽力的强磁性矿物-磁铁矿,磁铁矿的粒径为PSD(准单畴)。加热过程中,含铁粘土矿物绿泥石分解生成新的磁铁矿,磁畴转变成MD(多畴),逐步加热的K-T曲线表明,利用K-T曲线分析含有大量有机质成分弱磁性物质的磁性特征具有一定的指导作用,泥炭样品受热生成的磁性矿物的类型与数量不仅受加热的最高温度控制,同时在加热到不同温度时由于有机质对磁性矿物的还原作用表现出差异性,使得泥炭样品加热到不同温度后的转化、改造及最终生成物亦变得异常复杂。Sedimentary rock, some metamorphic rock, acidicrock and the sample dominated by peat or organic matter are all located in the weak magnetic measurement range. How to explain the low magnetic susceptibility in the point of magnetic mineral？ As the reliable atmospheric archive of the present and past, peat sediments have high organic matter and low magnetic susceptibility, What is the dominant magnetic properties of the mineral. Whether K -T curve can help to recognize the magnetic minerals and magnetic properties in the peat, whether it al- so helps to understand the sources of magnetic minerals and how organic matter affects magnetic minerals under the influence of the temperature. To understand these, the paper conducted magnetic investigation to a surface peat sample on the Altay Mountains, Xinjiang Uygur Autonomous Region, China. Mainly based on the K -T curve, combined with the J - T curve, hysteresis parameter and XRD experiment, the paper made thermomagnetic experi- ment to distinguish magnetic property of weak magnetic substance which contain plenty of organic matter. The heat- ing and cooling K -T curves are reversible, indicating that crystalloid structure and magnetic domain do not change before the samples are heated to 200 ℃. The cooling lines of magnetic susceptibility all locate above the heating line after being heated to 300℃, 400 ℃, 500 ℃, 600 ℃separately and the changing extent escalates, which shows that more and more magnetic minerals come into being during the heating. When being heated from 0 ℃ to the maximum temperature of 700 ℃, the most distinctive decreasing of magnetic susceptibility occurs at around 580 ℃ and then quickly decreases to 0 ℃, which indicates the presence of magnetite and it demonstrates the unblock- ing temperature of magnetite. During the cooling process from 700 ℃ to 500℃, magnetic susceptibility slowly de- creases, denoting the magnetite probably transforms. For the J - T curve, when the sample starts to be heated, the magnetization slowly decre

关 键 词：泥炭 K—T曲线 温度 磁铁矿 

分 类 号：P579[天文地球—矿物学]