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61.
基于1980年、2005年和2015年3期区域精密水准网观测资料,利用线性动态平差模型计算获取大别山地区水准网长期垂直运动速度场图像。研究发现,淮河平原地表下沉较为严重,大别山呈现弱隆升趋势运动,长江谷地边缘地区较大别山区呈现明显的隆升运动。跨郯庐断裂带水准剖面结果显示,垂直运动与地形呈负相关和弱相关。 相似文献
62.
该文以中国南方一厚碳酸盐岩覆盖区的RVSP三维地震勘探实例,对RVSP三维地震勘探观测系统和数据采集参数的确定、地面等效处理和波场分离等关键处理技术及地质效果进行了阐述和分析,说明了RVSP在克服表浅层复杂地质条件及环境条件对资料的影响及提高地震资料的分辨率有其特定的优势,同时也提出了RVSP三维地震在采集和处理过程中的难点。 相似文献
63.
于2011年5-8月,选择腾格里沙漠东南缘人工固沙植被区藻类、藓类和混生结皮覆盖的土壤为对象,研究了极端降雨量(降雨量44.7 mm、强度0.04 mm,min-1)、极端降雨强度(降雨量8.3 mm、强度0.55 mm·min-1)及普通降雨(降雨量16.3 mm、强度0.02 mm·min-1)条件下的碳释放过程.碳释放量的测定采用Li-6400-09土壤呼吸室,降雨结束后立即开始观测,直到呼吸速率恢复到降雨前水平时停止观测.结果表明:极端降雨(降雨量和降雨强度)结束初期藻类和混生结皮覆盖土壤的呼吸速率受到明显抑制,藻类结皮覆盖土壤呼吸速率分别为0.12 μmol·m-2·s-1和0.41 μmol·m-2·s-1,混生结皮覆盖土壤呼吸速率分别为0.10 μmol·m-2·s-1和0.45μmol·m-2·s-1;而极端降雨对藓类结皮覆盖土壤的影响不明显,呼吸速率分别为0.83 μmol·m-2·s-1和1.69μmol·m-2·s-1.这说明处于演替高级阶段的藓类结皮能够很好地应对短期的极端降雨事件. 相似文献
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66.
天津市滨海地区地面沉降灾害风险评估与区划 总被引:6,自引:2,他引:6
文章对1985~2006年累计地面沉降量及近几年地面沉降速率进行分析和叠加评价,完成天津市滨海地区地面沉降灾害危险性分区图;以人口密度和单位面积GDP为指标进行易损性分析;从每km2水准测量km数和地下水压采量占开采量百分比两方面考虑防灾减灾能力;在此基础上,借助GIS空间分析方法,将危险性分区图、易损性分区图和防灾减灾能力分区图进行叠加分析,完成天津市滨海地区地面沉降灾害风险区划图,分为低风险区、较低风险区、中等风险区、较高风险区、高风险区5等。 相似文献
67.
Xingping Wen Xiaofeng Yang Guangdao Hu 《Journal of the Indian Society of Remote Sensing》2011,39(2):193-201
Urban heat island (UHI) effect has a close relation to land covers type. This paper investigates the relationship between
land cover ratio and UHI in Guangzhou, south of China using remote sensing and automatic weather stations data. The temperature
data were obtained by Automatic weather stations (AWS) of Guangzhou in October, 2004, at the same time with the CBERS remote
sensing image acquired. Firstly, the hourly mean temperature was computed from hourly AWS data. Secondly, the CBERS remote
sensing image was classified using support vector machine (SVM) and land covers classification were output. Thirdly, the classification
result was overlapped with a round buffer with 1.5 KM radius centered on the AWS, and then the land cover ratio, Edge Density
(ED) and Mean Fractal Dimension (MFRACT) of buffers were computed out. Finally, the correlation coefficient between hourly
mean temperature and land cover ratio, ED and MFRACT was calculated. It concluded that UHI intensity was heavier during nighttime
than daytime. Stations with higher vegetation ratio and higher ED had lower heat island effect. On the contrary, stations
with higher impervious ratio and lower ED had more serious heat island effect. The positive–negative of correlation coefficient
between hourly mean temperature and vegetation ratio during 11:00–17:00 h (local time) was opposite to that during other time.
ED was negatively correlated with hourly mean temperature except during 11:00–17:00 h. On the contrary, MFRACT was positively
correlated with hourly mean temperature. It implied that fragmentations of patches were favorable to UHI alleviation, and
complexities of patch were unfavorable factors. 相似文献
68.
河北省县域乡村韧性测度及时空演变 总被引:1,自引:0,他引:1
目前中国城乡变化剧烈,乡村地区面临的风险加剧,如何有效提升乡村韧性,成为亟须探索的重要议题.通过构建乡村韧性分析框架,对1996-2016年河北省县域乡村韧性的时空分异格局及演变过程进行测度与分析,研究结果表明:1)县域乡村综合韧性经历了从小幅提升到明显增强的演化过程,且县域间乡村综合韧性差距呈现先上升再下降的趋势;在生态环境和经济发展水平两个主导因素影响下,县域乡村综合韧性总体呈现以"阜平县—平泉市"一线为界,东南高、西北低的分布格局.2)县域乡村综合韧性存在空间正相关性,空间集聚程度呈现先弱后强的变化态势;县域乡村综合韧性正向集聚程度呈现先强后弱的趋势,邻域单元韧性的差距则有所扩大.该研究可在一定程度上丰富乡村韧性与乡村可持续发展理论以及乡村韧性的测度方法,弥补现有研究尺度的不足,并为明确乡村的发展优势和薄弱环节、提升乡村地域系统的韧性潜力、推动乡村治理路径的创新提供参考. 相似文献
69.
Numerous lakes in western China are excellent sites for understanding environmental change. However, what dominates rare earth element(REE) variations are still under debate in the lake environmental research. In this study, we selected 28 surface sediment samples from 17 lakes(i.e. largescale lakes, small water bodies, etc.) in the QinghaiTibet Plateau and Xinjiang area. These samples were analyzed to reveal the behavior of the REEs and major elements. These REE patterns are characterized by light rare earth element(LREE) enrichment, weak Ce anomaly(0.84-0.98, 0.94 on average) and negative Eu anomaly(0.53-1.00, 0.67 on average). The homogeneous REE patterns may reflect similar REE of the source lithologys. However, the REE abundances showed some significant differences. In this study, water chemistry data analyses inferred that the highly REE values appear possibly in the saltwater lake, and also related to carbonate mineral, whereas p H played a minor role in REE concentrations. In large-scale lakes(e.g. Lake Bosten and Lake Ulungur), the results showed that the relatively larger REE values are in the margins of lakes. Moreover, lower REE contents are towards the central region. Comprehensive study suggested that five major factors control the REE contents:(1) The REE tends to increase with the increase of the weathering intensity.(2) Likewise, heavy mineral(i.e. rutile, anatase, zircon, etc.) are probably primary in these sediments because they are highly enriched in the REE.(3) The contribution of Fe-Mn oxides is significant in sediments because their concentrations highly correlate with the REE.(4) The carbonate mineral(mainly calcite) played a significant role on the REE values in the lakes because the REEs are incorporated into the carbonate minerals generating the low REE concentrations.(5) Major element analysis, mineral analysis, and grain-size data analysis showed that the REE distribution is chiefly influenced by finer grain-size component of lake sediments due to the decreasing proportion of quartz and feldspar than coarser one. Moreover, the clay minerals in finer grain-size sediments can highly absorb the REE. 相似文献
70.