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排序方式: 共有75条查询结果,搜索用时 31 毫秒
1.
腾格里沙漠晚更新世以来湖相沉积年代学及高湖面期的初步确定 总被引:20,自引:1,他引:20
张虎才 《兰州大学学报(自然科学版)》1997,(2)
对腾格里沙漠古湖泊沉积和地貌的考察及对典型代表剖面初步研究结果表明,一个连续而巨大的淡水湖泊高水位形成于距今3.9~3.6万年前.在距今3.3~2.3万年期间,腾格里沙漠西北部曾存在一面积至少达16200km2、水深25m(白碱湖,最大水深超过60m,分布于大海子一带)的淡水湖泊.大量的瓣鳃类、腹足类化石及介形类化石组合的存在表明该时期湖泊水温不低于10℃,由此把该时期的湖泊暂且称“腾格里大湖”(MegalakeTengger) 相似文献
2.
Temporal-spatial dynamics of distribution patterns of microorganism relating to biological soil crusts in the Gurbantunggut Desert 总被引:1,自引:0,他引:1
WU Nan WANG Hongling LIANG Shaoming NIE Huali ZHANG Yuanming 《科学通报(英文版)》2006,51(A01):124-131
Biological soil crusts serve as an important biological factor contributing to the sand fixation. This study was conducted to investigate the temporal-spatial variability of microorganism in crusts relating to locations, soil layers of sand dunes and seasons. At moss-dominated inter-dune areas, higher soil nutrient and water concentrations were likely to maintain the microbial activities. Bacteria showed the highest capabilities of settlement and growth in inter-dunes in both spring and autumn. Soil water content reached the highest value in soil crusts in the inter-dune areas, especially in spring. Variations of quantities of actinomyces and fungi basically showed the consistent trend in different locations of sand dunes. With the deepening of soil layers, vertical distribution of quantities of each microorganism group showed different characteristics because environmental factors fluctuated in both spring and autumn. Among different microorganism groups, bacteria were predominant, actinomyces the next and fungi the least in both spring and autumn in all soil layers (0-20 cm). The proportion of bacteria and soil water content were higher in spring than those in autumn in all soil layers (0-20 cm). No consistent trends were found in actinomyces and fungi. The results showed that the quantities of microorganisms were significantly positive correlated with organic matter content, soil water content, total N, total P, available P, available K, pH, electrical conductivity, total salt content,catalase, urease, phosphatase and alkaline phosphatase. 相似文献
3.
基于气象数据、MODIS遥感影像数据和NCEP再分析资料, 利用HYSPLIT模型模拟2000—2019年毛乌素沙地上空不同海拔高度(500, 1000和1500 m)各季节沙尘暴的前向轨迹, 并与遥感影像识别出的沙尘信息进行比较, 识别毛乌素沙地沙尘暴的影响范围。结果显示: 1) 在过去的20年中, 共有143个沙尘暴月和387个沙尘暴日, 并且 2004 年以来, 毛乌素沙地发生沙尘暴的频率逐渐降低; 2) 季节性气候条件对毛乌素沙地沙尘暴的移动路径有很大的影响, 春季沙尘暴发生频率较高, 秋季发生频率最低; 3) 受毛乌素沙地沙尘暴影响的国内地区主要包括陕西省北部、山西省北部、河北省北部和中部、山东省北部和中部、北京市、天津市、内蒙古自治区东部以及东北三省, 国外受影响的地区有朝鲜、日本北部以及俄罗斯与我国交界处, 受影响的海域有渤海、黄海北部和日本海西北部。遥感影像与HYSPLIT模型的比较提供了一种对沙尘运输、扩散和沉积过程进行验证和加深了解的有效工具, 研究结果可以为防灾减灾决策及沙源地治理提供科学的参考依据。 相似文献
4.
不同放牧方式对半荒漠草原土壤理化性质的影响 总被引:1,自引:0,他引:1
本文以中蒙两国相邻地带小针茅半荒漠草原为研究对象,对游牧和定居放牧条件下土壤理化性质进行了研究,研究结果表明:蒙古国传统游牧区和内蒙古定居放牧区土壤含水量分别为10.06%、6.71%,两者存在显著差异(P<0.05);蒙古国游牧区砂粒含量明显少于定居放牧区,分别为56.27%和84.23%,两者存在显著差异(P<0.05);游牧区除土壤全钾外其它养分指标均高于定居区,而pH定居>游牧. 相似文献
5.
Loess in the Tian Shan and its implications for the development of the Gurbantunggut Desert and drying of northern Xinjiang 总被引:8,自引:0,他引:8
Xiaomin Fang Zhentao Shi Shengli Yang Maodu Yan Jijun Li Ping’an Jiang 《科学通报(英文版)》2002,47(16):1381-1387
Eolian loess is widely distributed on the various geomorphic surfaces between 700–2400 m a.s.l. on the northern slope of the
Tian Shan. It is formed in a synchronous manner with dust transported from the Gurbantunggut Desert in the Junggar Basin.
The thickest section of loess was found in the Shawan and Shihezi regions. Paleomagnetic and climatic proxy analyses of over
71 m of a loess-paleosol sequence on the highest terrace of the Qingshui He (River) in the Shawan show that the paleomagnetic
Bruhues/Matuyama (B/M) boundary lies at the bottom of paleosol S8, at a depth of 69.5 m, and the bottom of the sequence was
estimated to be ∼0.8 Ma. This implies that the extremely dry climatic conditions in the Junggar Basin and the initial Gurbantunggut
Desert were present at least by 0.8 Ma. High-resolution grain size series demonstrate that this area and desert expansion
experienced two dramatic periods of desert expansions that occurred at ∼0.65 Ma and 0.5 Ma, respectively; and the subsequent
continuous enhancement led to the environment presently observed. This tremendous environmental effect, caused by large-scale
expansion of the desert and arid region of inner Asia, might be an important driving force for the global temperature drop
that occurred in the mid-Pleistocene. 相似文献
6.
B.Wünnemann 《科学通报(英文版)》2002,47(23):1946-1956
Comprehensive field investigations and laboratory analyses show that palaeolakes, including fresh- mesohaline water Megalake Tengger and other semi-con- nected, isolated water bodies, during late Pleistocene covered an area of more than 20000 km2, which is more than half of the Tengger Desert in NW China. Stratigraphic correlation and chronological evidence indicate that before ca. 42000 aBP the area was more arid. The palaeolakes started to develop around 40000 uncal. 14C aBP but until 37000 14C aBP their scope was limited. High water levels established from 35000 14C aBP lasted until 22000 14CaBP. Lake levels regressed between 22000 and 20000 14C aBP but transgressed from 20000 to 18600 14C aBP. Subsequently, water level declined further and the Megalake Tengger finally desiccated at around 18000 14C aBP. Megalake Tengger possessed a fresh-mesohaline water property, implying that the regional precipitation increased significantly. During the period of Megalake Tengger, the climate was warmer-humid than present. The annual rainfall was 250 to 350 mm more than that of today and the temperature was 1.5 to 3.0℃ higher. 相似文献
7.
文章探讨了在新疆北山地区特殊地质环境下,采用现场X射线荧光测量找金的方法技术问题。提出适合于该区快速找金的X射线荧光找矿最佳指示元素为铁、铜、砷,铁和铜的X射线荧光异常出现在垂直于金矿(化)体走向的两侧,砷的X射线荧光在金矿(化)体上呈现异常。 相似文献
8.
9.
基于MODIS数据的巴丹吉林沙漠冬季暖岛空间分布特征及其研究 总被引:1,自引:0,他引:1
使用遥感与地理信息系统技术,利用2012年12月-2013年2月的MODIS地表温度数据产品对巴丹吉林沙漠地区冬季地表温度进行研究.将巴丹吉林沙漠分为湖泊区、沙漠外围区和沙漠周边区3个区域,旨在对3个区域的白天和夜晚地表温度进行研究对比.结果显示位于巴丹吉林沙漠腹地的湖泊区冬季白天和夜晚平均地表温度为6.10?C和-14.37?C,沙漠外围区分别为4.25?C和-15.44?C,沙漠周边区分别为4.07?C和-14.29?C,存在沙漠腹地湖泊区地表温度明显高于沙漠其他区域的"暖岛效应",其形成机制可能与远程地下水补给湖泊群有关. 相似文献
10.
Through stratigraphy and chronology studies on Hongshui River section located at the southern vicinity of Tengger Desert,
and based on the analysis results of TOC, TIC, elements, stable oxygen isotope that possess a high resolution of 40–50 a,
the paleaoclimatic change history during last 8 000–3 000 a has been reconstructed. 相似文献