黄淮海平原耕地功能演变的时空特征及其驱动机制（英文）

Using counties as the basic analysis unit,this study established an evaluation index system for farmland function(FF) from economic,social,and ecological perspectives.The method combining entropy weighting and multiple correlation coefficient weighting was adopted to determine the weights,and the FF indices were calculated for each county.Subsequently,the spatio-temporal characteristics of farmland function evolution(FFE) were analyzed and the coupled relationships between the sub-functions were explored based on a coupling coordination model.At the same time,the dynamic mechanism of FFE was quantitatively analyzed using a spatial econometric regression analysis method.The following major conclusions were drawn:(1) The farmland economic function generally exhibited a declining trend during 1990–2010,and it is essential to point out that it was stronger in underdeveloped and agriculture-dominated counties,while it continuously weakened in developed areas.Farmland social function decreased in 60.29% of the counties,whereas some counties,which were mostly located in north of Zhengzhou and west of Dezhou and Cangzhou,Yantai,and Weihai,clearly increased.A dramatic decline in farmland ecological function occurred around Beijing,Tianjin,and Jinan.Areas located in the northern part of Henan Province and the central part of Shandong Province saw an increase in ecological function.(2) There was a significant spatial difference in the coupling degree and coordination degree of the sub-functions,and the decoupling phenomenon highlighted this.The changes in social function and ecological function lagged behind economic function in developed areas,but these were highly coupled in some underdeveloped areas.(3) FFE in the Huang-Huai-Hai Plain(HHHP) is resulted from the comprehensive effects of regional basic conditions and external driving factors.Furthermore,the transitions of population and industry under urbanization and industrialization played a decisive role in the evolution intensity and direction of farmland sub-systems,including the economy,society,and the ecology.According to the results mentioned above,promoting the transformation from traditional agriculture to modern agricultureshould be regarded as an important engine driving sustainable development in the HHHP.Taking different regional characteristics of FFE into account,differentiated and diversified farmland use and management plans should be implemented from more developed urban areas to underdeveloped traditional agricultural areas.     

浅析提高工业用地利用效益的对策

平湖市是一个土地资源小市,全市陆域面积仅537平方公里,2011年实现生产总值395亿元,人均生产总值超8万元,     

重力观测在中国地壳运动观测网络中的作用

介绍了第一期“中国地壳运动观测网络”观测得到的重力变化图像和1996年2月3日丽江7．0级地震震中及附近重力测点的重力变化。初步探讨了青藏高原隆升与重力变化的关系。     

对城镇数字地籍调查几个关键问题的探讨

在数字地籍调查中,宗地依附的现状地物发生变化的情况很普遍,对于依附现状地物发生变化的宗地处理情况,各地作业也没有统一的方法。本文结合整个城镇数字地籍调查项目的规划和实际作业中的一些例子,对城镇数字地籍调查过程中的三个关键问题,即"宗地原始库整理(各种类型注销宗地情况分析)"、"宗地与现势地形的匹配"、"构建与宗地有关三个面的用处"给出自己的分析和解决方法,供探讨。     

固体潮对地球重力场时变特征影响的时间频谱公式

精密和详细测定地球重力场及其时间变化，是目前卫星重力测量的主要课题。基于固体潮研究的最新成果，研究了固体潮对地球重力场时变特征的影响。不同于IERS2003采用的Cartwright和Tayler(1971)的引潮力位(TGP)展开，而是利用郗钦文的TGP展开，给出了固体潮对地球重力场时变特征影响的理论公式，并考虑到4阶潮汐的效应，精度可达到1011^-11ms^-2量级，同时采用最新的TGP展开数据重新计算了固体潮Love数相对频率特性对地球引力场的影响，并考虑了较多的潮波项，最后对重力数据归算中的永久性潮汐的处理进行了总结和说明。     

矿物原生包裹体人工合成的实验研究

一、前言 矿物包裹体作为成矿流体的标本,为地质找矿、成矿理论、地球化学研究提供了成矿流体的温度,压力、盐度、密度、气液相成份、Eh、pH值及稳定同位素等方面证据,已经形成了一门新的学科,在地质学各领域中得到普遍的应用和承认。 作为独立的新学科,有许多问题有待深入进行研究,其中最突出的问题就是包裹体测量数据是否反映了成矿流体的真实情况?包裹体形成的三大假说是否成立?这些问题仅仅通过天然矿物包裹体本身研究是无法解决的。为此,我们在已知条件下,用人工合成矿物包裹体的办法,为解决上述问题提供了有效的途径。     

基于星间加速度法精确和快速确定GRACE地球重力场

本文基于星间加速度法(IRAM),利用预处理共轭梯度迭代法(PCCG)开展了地球重力场恢复的模拟研究.第一,通过9点Newton-Gregory插值法得到星问加速度,并联合星间距离、星间速度和星间加速度建立了卫星观测方程.第二,在120阶处,恢复GRACE-IRAM累计大地水准面的精度为7.215 cm.第三,分析了在...     

基于新型能量插值法精确建立GRACE-only地球重力场模型

本文基于新型能量插值法,利用美国喷气推进实验室(JPL)公布的2008年的GRACE-Level-1B实测数据,反演了120阶GRACE地球重力场.首先,由于GPS轨道测量精度相对较低,通过将K波段测距仪高精度的星间距离观测量插值引入双星动能差中,进而建立了新型能量插值卫星观测方程.其次,详细对比分析了2点、4点、6点和8点能量插值观测方程对地球重力场反演精度的影响.研究结果表明:基于最优的信噪比,6点能量插值公式有利于提高120阶GRACE地球重力场的反演精度.最后,基于美国、欧洲和澳大利亚的GPS/水准观测数据检验了本文新建立的WHIGG-GEGM03S地球重力场模型的正确性和有效性.     

联合卫星重力和卫星测高确定南极绕极流

联合基于GRACE重力卫星观测资料恢复的重力场模型(EIGEN-GL04S1)和卫星测高推求的平均海面高模型(KMSS04)来构造南极绕极流区域的平均海面动力地形,并利用小波滤波方法去掉短波及噪声信号,进而推算大、中尺度的绕极流。与非卫星重力场模型、同化资料及海洋水文资料确定相应结果的验证分析表明:基于新的卫星重力场模型推算的南极绕极流区域的海面动力地形、PF、SAF和表层流场等都与海洋学结果相吻合,且局部特征更加清晰。表明卫-卫跟踪重力卫星计划确定的地球重力场模型较之以前存在的重力场模型在中长波部分精度有较大提高,从大地测量(从空间)角度来探测南极绕极流已达到较高的精度。