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Pedogenesis and its effects on the natural remanent magnetization acquisition history of the Chinese loess.

机译:黄土的成岩作用及其对天然剩余磁化习性的影响。

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The thick (100--300 m) Chinese loess/paleosol sequences are good archives for both paleoclimate and paleomagnetism. Previous studies have shown that the large-scale Milankovitch cycles can be recorded by the Chinese loess. However, there exist some barriers against further quantitative and accurate interpretation. The most specific one is that pedogenesis has strongly altered (overprinted) not only the acquisition history of the natural remanent magnetization (NRM) but also the paleoclimatic proxies (e.g. low-field magnetic susceptibility). Therefore, this study aims to solve this problem by quantifying the effects of pedogenesis on the loess NRM acquisition history and further to probe the mechanism of susceptibility enhancements. The thesis is divided into three parts: Part I (Chapters 2 to 7) proposes several new techniques in rock magnetism to determine the exact carriers of various magnetic parameters, e.g., susceptibility, anhysteretic remanent magnetization (ARM), NRM and the corresponding Characteristic remanent magnetization, etc; Part II (Chapters 8 and 9) focuses mainly on the mechanism of low-temperature oxidation and its effects on the magnetic signals; and Part III (Chapters 10 and 11) discusses the mechanism of susceptibility enhancements. The main conclusions and contributions of this thesis are: (1) The enhancement of magnetic susceptibility is dominated by single-domain (SD) maghemite of pedogenic origin (>50%) instead of the pedogenically produced superparamagnetic (SP) particles; (2) For loess sample, its NRM and ChRM is carried by aeolian coarse-grained partially oxidized magnetite (CG-POM). However, this primary remanence can be easily masked by the secondary Chemical remanent magnetization (CRM) carried by pedogenic maghemites; (3) Due to low-temperature oxidation, the aeolian CG-POM has a much higher coercivity than the pedogenic fine-grained particles; therefore, alternating field (AF) demagnetization is more efficient to separate the primary detrital remanent magnetization (DRM) from the secondary CRM than conventional thermal demagnetization; and (4) The enhancement of susceptibility is sensitive to precipitation more than to temperature variations.
机译:中国黄土/古土壤层厚(100--300 m)是古气候和古磁性的良好档案。以前的研究表明,中国黄土可以记录大规模的米兰科维奇周期。但是,存在一些阻碍进一步定量和准确解释的障碍。最具体的一个是,成岩作用不仅改变了自然剩磁(NRM)的获取历史,而且还改变了古气候的代理人(例如低磁场磁化率)的记录(套印)。因此,本研究旨在通过量化成土作用对黄土NRM采集历史的影响来解决该问题,并进一步探索敏感性提高的机制。本文共分为三个部分:第一部分(第2章至第7章)提出了几种岩石磁学的新技术,用于确定各种磁参数的精确载流子,例如磁化率,磁滞剩磁(ARM),NRM和相应的特征剩磁。磁化等;第二部分(第8章和第9章)主要关注低温氧化的机理及其对磁信号的影响。第三部分(第10章和第11章)讨论了磁化率增强的机制。本论文的主要结论和贡献是:(1)磁化率的增强主要由成岩成因的单畴(SD)磁赤铁矿(> 50%)代替,由成岩作用产生的超顺磁(SP)颗粒主导; (2)对于黄土样品,其NRM和ChRM由风成的粗粒部分氧化磁铁矿(CG-POM)携带。但是,这种初生剩磁很容易被成岩磁赤铁矿携带的次生化学剩磁(CRM)所掩盖。 (3)由于低温氧化,风成粒CG-POM的矫顽力比成岩细粒高得多;因此,与传统的热消磁法相比,交变磁场(AF)消磁法能更有效地将初级碎屑剩磁化(DRM)与次级CRM分离。 (4)磁化率的增强对降水的敏感性大于对温度变化的敏感性。

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