抚松井水温动态特征分析

统计分析了抚松井2007年6月1日至2010年12月30日水温数字化观测资料,结果显示抚松井水温动态类型表现为：长期动态特征为上升漂移型;短期动态特征为短周期型,并结合环境和水文地质情况对水温动态的影响因素进行了初步的分析。     

X射线技术在安检领域的应用

X射线技术是一种成熟且应用非常广泛的安检技术,主要包括X射线透射法、双能X射线法、X射线背散射法和计算机断层扫描法等。其成像原理虽略有不同,但都是利用X射线与物质作用来提取物品的物理特征,从而达到安全检查的目的。在实际应用中,各类X射线技术都存在各自的缺点和不足,造成实际安检存在漏报、误报等问题,为解决这些问题,综合应用各类技术可能是一个有效的解决办法。     

田岗断层产状的确定方法

搞清断层赋存状态对矿井安全生产至关重要。针对目前以范围表示方法确定断层产状存在精度不足的问题,山东崔庄煤矿通过在井下施工断层探孔,探明了田岗断层地质层位关系等情况,并运用平面投影法和矿体几何要素较准确地确定了田岗断层的产状要素,包括断层倾角、断层落差和断层走向等,从而取代了通常对断层产状较模糊的范围表示法。本研究方法原理简单,易于掌握,其计算结果比原有地质资料更加准确可靠。      

一类非线性波动方程的新的精确解

为了寻求一类著名的非线性波动方程utt-kuxx+pu+qu2+su3=0的新精确解。利用齐次平衡法的思想与改进的G′/G展开法,通过对解的形式的巧妙构造可以将方程约化为一组非线性方程组,借助于数学软件Maple强大的符号计算功能得到了方程包括双曲函数解、三角函数周期解、有理数解在内的3种形式的精确解。同时给出了其中一组情况的数值模拟图。这些解对正确理解方程在自然科学中的物理意义具有重要的作用。     

利用海图数据与卫星影像计算海湾纳潮量——以胶州湾为例

以胶州湾为例,尝试获取胶州湾的三维地形,并利用海湾高、低潮所容纳的海水体积之差计算海湾纳潮量。计算结果表明:胶州湾1992年纳潮量为9.8×108 m3,2005年胶州湾纳潮量为8.9×108 m3,胶州湾纳潮能力下降0.9×108 m3。     

如何评定并提高城市土地利用效率

一、背景 当前我国城市化进程进入加速发展时期,城市化必须以土地作为载体,而我国的城市土地利用面临着世界上少有的严峻环境。一方面,国家目前正处于工业化和城市化的加速发展阶段,城市用地扩展是发展经济和提高人民生活质量的必然要求;     

利用重砂寻找原生矿床

在森林沼泽覆盖区利用重砂寻找原生矿床,曾是我省地质找矿工作的重要手段之一。在我省已完成的1：20万区域地质填图及部分1：5万地质矿产调查中,都曾系统地开展过重砂测量,     

重庆中坝遗址地层Na-Ca元素含量揭示的制盐业兴衰史

Based on dynastic period division and AMS ^14 C dating performed on the sedimentary layers at Zhongba and Yuxi sites,and also the analysis of Na,Ca and Mg of 201 sedimentary samples from Zhongba site and that of Ca and Na in 47 sedimentary samples from Yuxi by using an inductively coupled plasma-mass spectrometry（ICP）,we found that there were 35 time periods when the contents of Ca and Na were reversely correlated,i.e.whenever the content of Ca was the highest,the content of Na was the lowest,and vice versa. Among them,there were 21 time periods when the content of Ca was the highest,and Na was the lowest,indicating that there were about 21 prosperous periods of ancient salt production at Zhongba site since 3000BC.Other 14 time periods with the peak values of Na while the low values of Ca indicate 14 declined periods of salt production at Zhongba site since 3000BC.The conclusion obtained from the reverse relationship between Ca and Na contents in this paper is consistent with that＂the salt production at Zhongba site started in the new stone age,developed in the Xia and Shang dynasties,reached at the heyday in periods from the Western Zhou to the Han Dynasties,maintained stable to develop in the Tang and the Song dynasties,and gradually declined after the Song Dynasty because the sea salt were conveyed into Sichuan region,however,still had production in the 1970s-1980s＂,educed from archeological exploration.All the above mentioned results indicate that there is a reverse relationship obviously between the contents of Na and Ca in sediments at Zhongba site for ancient salt production,which can be used to reveal the process of rise and decline of ancient salt industry at Zhongba site.