地表移动破坏裂缝特征及其控制方法

通过分析地下开采的影响，黄土覆盖层变形裂缝规律，提出以开采方法和工艺方式来控制或减弱地表变形裂缝破坏程度，并在保护地表建筑物的前提下，最大限度回收“三下”呆滞煤炭     

流变力学原理在黄土滑坡研究中的应用

通过对黄土滑坡演变过程的分析、滑带土体流变性质及演变过程的讨论,论述了流变力学原理在黄土滑坡研究中应用的可行性,并探讨了流变力学在黄土滑坡研究应用中存在的问题,与同行商榷.     

短正合列的弱可裂

把短正合列的可裂推广到短正合列的弱可裂，并对弱可裂进行了等价刻画，最后还运用左弱可列证明了平坦模的一个充要条件。     

试论《化学教学论》教材的修订——从六大类中学化学教材内容的编排顺序谈起

现行《化学教学论》教材将典型教学示例放在化学教学原则之后，致使整本教材缺乏逻辑性，不符合当前创新能力培养的要求，不利于坚定师范生从事教育事业的信心，笔者认为应先讲教学示例、后授教学原则。     

黄土滑坡形变分析预报方法研究

基于黄土滑坡的变形特征和演化规律，利用滑体总形变量与滑坡演变过程形变量之间的逼近关系，建立了一种简单，实用的滑坡预报数学模型，其效果良好，为黄土滑坡时间预报由定性分析向定量评价提供了途径。     

关于指数丢番图方程x~2+(3a~2+1)~m=(4a~2+1)~n(英文)

应用Bilu,Hanrot和Voutier关于本原素因子的深刻理论及二次丢番图方程解的表示等方面的精细结果,完全解决了指数丢番图方程x2+(3a2+1)m=(4a2+1)n在3a2+1为奇素数或奇素数幂时的求解问题.     

关于湿陷性黄土试验方法的初步探讨

文章介绍了黄土湿陷性试验的两种试验方法,对黄土湿陷机理作了简要分析,并对双线法的误差及其修正进行了讨论。     

Iterative Method for Constructing Complete Complementary Sequences with Lengths of 2^mN

Complete complementary sequences are widely used in spectrum spread communications because of their ideal correlation functions. A previous method generates complete complementary sequences with lengths of N^nN （n,N ∈ Z^＋）. This paper presents a new iterative method to construct complete complementary sequences with lengths of 2^mN （m,N ∈ Z^＋）. The analysis proves that this method can produce many sequence sets that do not appear in sequence sets generated by the former method, especially shorter sequence sets. The result will certainly increase the application of complete complementary sequences in communication engineering and related fields.     

A recording phase lag between ocean and continent climate changes: Constrained by the Matuyama/Brunhes polarity boundary

The Matuyama/Brunhes polarity boundary (MBPB) is recorded in Chinese loess L8, which is associated with the glacial period. It is proved that loess L8 is capable of recording earth’s secular variation, and the lock-in depth in Chinese loess is no more than that of marine sediments. Comparison with the location of MBPB in Chinese loess and marine sediments, it is put forward that there is a recording phase lag between ocean and continent climate changes.