提高机采水平的配套技术及应用

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海底孔内水合物观测系统与钻井实施

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矿业权实地核查测量技术方案探讨

阐述了葫芦岛地区矿业权实地核查工作的目的、意义和工作依据,并对矿业权实地核查方法、矿权测量、数据整理、数据库建设等具体的工作方法和技术要求进行了探讨.     

DZJ2激光垂准仪使用方法及指标的校正

介绍了DZJ2激光垂准仪的性能及基本指标的校正方法,为用户在使用DZJ2激光垂准仪过程中几种基本指标参数的校正提供参考.     

连续运行参考站系统的建设及其在测量中的应用

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常用全站仪的电子校正方法

介绍了常用全站仪基本指标的校正方法,为用户在使用全站仪过程中保证仪器的精度提供参考。     

立体测绘型双翼民用无人机航空摄影系统的实现与应用

按照领域专用、性价匹配的思想,设计并实现了一套满足小区域大比例尺地形图立体测绘要求的无人机航空摄影系统.该系统以双翼无人机为遥感平台,以数字相机为传感器,配置3轴稳定云台,直接获得数字航空影像,具有自主飞行、低空作业、无需机站支持、起降距离短、滑翔性能好等特点.系统包括双翼无人机、飞行自动控制与安全、CCD数字相机、稳定云台、空地无线通讯、地面站和数据处理等7个子系统.分别介绍了系统的总体结构和各子系统的技术状况;分析和比较了系统的GSD、像点移位、基高比等关键参数在保证成像质量和成图精度方面的合理性;报告和展示了系统在广州新客站、丹江口文物考古测量工程的试验情况和部分成果;最后对系统的改进提出了建议.     

地理信息公共服务平台的总体技术设计研究

国家地理信息公共服务平台建设与运行维护是一项超大型地理信息工程。为了切实做好统筹规划、统一设计、规范建设、分步实施,国家测绘局组织开展了总体技术设计研究,制订了技术设计指南。本文介绍了国家地理信息公共服务平台总体设计的基本思路和总体架构。     

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Distribution patterns of chlorophyll <Emphasis Type="Italic">a</Emphasis> in spring and autumn in association with hydrological features in the southern Yellow Sea and northern East China Sea

Two field studies were conducted to measure pigments in the Southern Yellow Sea (SYS) and the northern East China Sea (NECS) in April (spring) and September (autumn) to evaluate the distribution pattern of phytoplankton stock (Chl a concentration) and the impact of hydrological features such as water mass, mixing and tidal front on these patterns. The results indicated that the Chl a concentration was 2.43±2.64 (Mean ± SD) mg m^?3 in April (range, 0.35 to 17.02 mg m^?3) and 1.75±3.10 mg m^?3 in September (from 0.07 to 36.54 mg m^?3) in 2003. Additionally, four areas with higher Chl a concentrations were observed in the surface water in April, while two were observed in September, and these areas were located within or near the point at which different water masses converged (temperature front area). The distribution pattern of Chl a was generally consistent between onshore and offshore stations at different depths in April and September. Specifically, higher Chl a concentrations were observed along the coastal line in September, which consisted of a mixing area and a tidal front area, although the distributional pattern of Chl a concentrations varied along transects in April. The maximum Chl a concentration at each station was observed in the surface and subsurface layer (0–10 m) for onshore stations and the thermocline layer (10–30 m) for offshore stations in September, while the greatest concentrations were generally observed in surface and subsurface water (0–10 m) in April. The formation of the Chl a distributional pattern in the SYS and NECS and its relationship with possible influencing factors is also discussed. Although physical forces had a close relationship with Chl a distribution, more data are required to clearly and comprehensively elucidate the spatial pattern dynamics of Chl a in the SYS and NECS.