利用异常元素水平分带序列评价矿床剥蚀程度——以兰家、八台岭、官马金矿为例     

康太翰  于洪顺 《吉林地质》1997,(1)

本文利用异常元素组合和综合垂向分带序列一致的同类型矿床具相同的异常元素水平分带，但矿体不同垂直截面上异常元素具有不同的水平分带的特征规律，来评价矿床的剥蚀程度  相似文献   

基于MODIS积雪覆盖产品的中国天山积雪时空分布特征研究     

侯小刚  李帅  张旭  陈雪华  崔宇 《沙漠与绿洲气象(新疆气象)》2017,11(3):9-16

利用2002-2016年MODIS逐日积雪遥感产品(MOD10A1、MYD10A1),采用日产品合成法、临近日分析法、空间滤波法和相邻时间合成法,生成天山山区逐日晴空积雪遥感产品数据集,研究分析了天山山区积雪时空分布特征。结果表明：近15a,天山山区平均积雪覆盖面积变化不明显,呈略微减少趋势,但主要表现为年际间的波动变化;分季节来看,天山山区积雪覆盖面积冬季 > 秋季> 春季 > 夏季;积雪面积从9月开始积累,1月达到峰值,占天山总面积的50±25%,3月开始消融,8月达到最低值,仅占天山总面积的为3.5±2%。;天山山区大部分区域积雪开始时间在第300天之后,积雪结束时间在第40~150天左右,海拔较高的区域积雪开始时间较早;天山山区平均积雪日数小于60天的不稳定积雪区主要分布在天山南坡、北坡边缘地带,占整个天山面积的44.57%,平均积雪日数在60~300天之间的区域占比为53.4%,主要分布在天山中部和北坡部分区域,平均积雪日数大于300天的永久积雪区,主要分布在海拔3800以上区域,占天山面积的2.03%。  相似文献   

Lack of significant change in epiphyte biomass with increasing extent of measurement within seagrass meadows     

Tim N. Moore  Peter G. Fairweather 《Estuarine, Coastal and Shelf Science》2006,68(3-4):413

A significant consideration in defining patterns of ecological interest is determining at what spatial scales these patterns are apparent. We performed a mensurative experiment to determine the effect of how changing the extent of sampling, using a fixed grain (panning up), changed our measurements of seagrass epiphyte biomass at a variety of hierarchical spatial scales, ranging from approximately 0.1 m to 2.5 × 10⁵ m. The experiment was performed twice at two sets of nested locations, also capturing an element of seasonality within the spatial extents. While the two regions and their nested locations differed in terms of epiphyte biomass, and values did change over time, mean epiphyte values were invariant at the local scale. This indicates that at the local scale (≤100 m extent), we expect seagrass epiphyte biomass to be relatively homogenous. Contrary to theoretical predictions, we did not detect predictable changes in mean values of epiphyte biomass as sampling extent increased. The results of this study highlight the importance of recognizing the spatial dependence of patterns in heterogeneous environments.  相似文献   

旅游气候宜人度评价方法研究   总被引：1，自引：0，他引：1  

钱妙芬  叶梅 《成都信息工程学院学报》1996,(3)

提出一个较客观、定量的评价“气候宜人度”的数学模型。它综合的描述了气压、日照、降水、雾日、风速、气温、相对湿度和大气污染物浓度对气候宜人程度的影响。使气候宜人度在时间、空间上更具可比性。对旅游资源开发、淡旺季出现规律和旅游导向较客观、科学和实用。最后对四川旅游气候宜人度作了计算和分析  相似文献   

High-frequency radiation from earthquake sources in laterally varying layered structures     

V. &#;ervený  J. Pleinerová  L. Klime&#;  I. P&#;en&#;ík 《Geophysical Journal International》1987,88(1):43-79

  相似文献   

利用MODIS和ASAR资料估算青藏高原念青唐古拉山脉地区冰雪范围及厚度   总被引：3，自引：1，他引：3  

文军  Dai Mo  王致君  张堂堂  Humbert Louis 《冰川冻土》2006,28(1):54-61

利用可见光和微波卫星遥感资料分析了青藏高原念青唐古拉山脉地区冰雪范围和厚度的季节变化.结果表明:青藏高原念青唐古拉山脉地区冰雪范围的季节变化非常明显,2003年4月上旬、5月中旬、7月下旬和9月下旬的冰雪范围分别占选定研究区域的28.9%、69.9%、11.6%和14.7%.在选定的西布冰川区域,由微波遥感得到的冰雪厚度季节变化也非常明显,5月份厚度的数值最大,7月份最小.由于主动微波观测受地面高程、地形和夏季冰雪融化等因素的影响比较大,主动微波遥感在大面积估算冰雪厚度还有一定困难,有待将来作进一步的深入研究.  相似文献   

Evidence for a 55-50 ka (early Wisconsin) glaciation of the Cordilleran ice sheet, Yukon Territory, Canada     

Brent C. Ward  Jeffrey D. Bond 《Quaternary Research》2007,68(1):141-150

Cosmogenic ¹⁰Be ages on boulders of 54-51 ka (n = 4) on a penultimate Cordilleran ice sheet (CIS) drift confirm that Marine Oxygen Isotope Stage (MIS) 4 (early Wisconsin) glaciation was extensive in parts of Yukon Territory, the first confirmed evidence in the Canadian Cordillera. We name the glaciation inferred from the mapped and dated drift the Gladstone. These results are in apparent contrast to the MIS 6 (Illinoian) age of the penultimate Reid glaciation to the east in central Yukon but are equivalent to exposure ages on MIS 4 drift in Alaska. Contrasting penultimate ice extents in Yukon requires that different source areas of the northern CIS in Yukon responded differently to climatic forcing during glaciations. The variation in glacier extent for different source areas likely relates to variation in precipitation during glaciation, as the northern CIS was a precipitation-limited system. Causes for a variation in precipitation remain unclear but likely involve the style of precipitation delivery over the St. Elias Mountains possibly related to variations in the Aleutian low.  相似文献   

中国耕地与未来30年食物需求、保障及对策   总被引：22，自引：1，他引：22  

吴绍洪  李荣生 《地理科学进展》2002,21(2):121-129

在未来的 30年中 ,中国的人口将继续增长 ,至 2 0 30年达到峰值 1 6亿 ,净增 3亿左右。随着社会经济的发展 ,人民生活水平的提高 ,人均食物需求的量与质越来越高。届时中国食物的保障能力受到国际社会的普遍关注。中国到 2 0 30年 ,满足上述食物需求量 ,食物主要来自耕地的生产潜力和非耕地的食物替代生产两方面。在政策非常强有力、一切从保护耕地出发、严格控制耕地占用和维持动态平衡的条件下 ,到 2 0 30年 ,中国耕地面积可保持 1 31× 1 0 6 hm2。而中国到 2 0 1 0年、 2 0 30年年人均需求粮食分别为 42 0 kg和460 kg,这两个基期年分别需求粮食总量为 5 796× 1 0 8kg和 7360× 1 0 8kg。研究认为 2 0 1 0年、 2 0 30年中国耕地动态变化后食物保障能力分别在 93%和 87%。非耕地资源食物替代是补充食物生产和缓解耕地压力的重要途径。 2 0 30年其食物替代能力可达到 90 0 0 0×1 0 3t,其中草业 3380 0× 1 0 3t,木本粮油 1 70 0 0× 1 0 3t,水域 2 5 82 0× 1 0 3t,野生生物 1 340 0× 1 0 3t,非耕地的事物替代能力达到约 1 0 %。中国食物生产与发展的四个保证 ,一是有效的保护耕地政策 ,二是科学技术进步与科技投入 ,三是构建食物生产体系与保障体系 ,四是高效利用水资源的技术与措施。  相似文献   

The System Analysis and Reliability Evaluation of Rock Slopes1     

Luo Guoyu  Yan Changhong 《《地质学报》英文版》1994,7(4):451-468

Abstract The principal of preferred plane analysis is a new research view and model of rock slope engineering geology. It advocates that the rock slope stability, boundary conditions and failure model are controlled by preferred planes. Therefore, the problem of slope stability evaluation can be converted into the search for preferred planes and determination of preferred separating bodies. The organic combination of the deterministic model and the indeterministic model can be realized by applying the systems engineering principle and the research model and method of reliability analysis in the quantitative evaluation and prediction of rock slope stability. Finally, the paper presents the case studies of slopes of the Yangtze Gorge Project and the Ma'anshan openpit mine.  相似文献   

The glacial extent and glacial advance/retreat asynchroncity in East Asia during Last Glaciation     

ZHANG Wei  CUI Zhijiu  LI Yonghua 《地理学报》2005,15(3):293-304

New dates for last glacial cycle in Tibetan bordering mountains and in East Asia show the glacial extent during the early/middle (MIS3-4) stage is larger than that of the late stage (MIS2) in last glacial cycle. It is asynchronous with the Northern Hemisphere ice sheets maximum and changes in oceanic circulation that predominately control global climate. In research areas, three seasonal precipitation patterns control the accumulation and ablation of glaciers. The modes of the westerlies and the East Asian mountains/islands in and along the Pacific Ocean are favorable to glacier advance with mainly winter precipitation accumulation. There was a global temperature-decreasing phase in the middle stage (MIS3b, 54-44 ka BP), when the glacier extent was larger than that in Last Glaciation Maximum due to the low temperature combined with high moisture. It is revealed that the Quaternary glaciers not only evolved with localization, but also maybe with globalization. The latest studies show a fact that the developmental characteristics of glaciers in high mountains or islands along the western Pacific Ocean are not in accord with those inland areas. Therefore, it can be concluded that glacier development exhibits regional differences. The study validates the reasonableness of the asynchronous advance theory, and ascertains that both the synchronous and asynchronous advance/retreat of glaciers existed from 30 ka BP to 10 ka BP. It is not suitable to emphasize the synchronicity between global ice-volume and glacier change.  相似文献