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The study was to give a technique support for the plant of special maize in semiarid area.

为半干旱地区特用玉米种植提供技术支撑。

Otindag Sandland is one of the main sandlands and among the most seriously desertificated region in semiarid area of China.

浑善达克沙地是我国北方干旱半干旱区的主要沙地和严重荒漠化地区之一。

More than 100 species: arid and semiarid regions of N Africa, C, N, and W Asia, Australia, S Europe; 19 species in China.

超过100种:非洲北部,C,N 和W亚洲,澳大利亚,S欧洲的干旱和半旱的地区;中国有19种(2特有种)。

This phenomenon is widely distributed in arid and semiarid area.

中国西北广大地区地处干旱半干旱地区,风蚀严重地影响着这些地区的农业生产。

Through investigation on the Eh values of cinnamon soil,sierozem,brown desert soil in situ with new electrochemical methods and summarization of the same results of laterite,red soil and yellow brown soil,a horizontal zonal variation of oxidation-reduction characteristics in semi-humid,semiarid and arid areas from south China to north China is revealed.

用新的电化学方法原位考察了褐土、灰钙土、棕漠土、黑土、风沙土、灌淤土、盐土、碱土、亚高山草甸土、灰褐土、水稻土和旱地土壤的氧化还原状况。综合已有原位测定结果,地带性土壤的电位由南向北的空间分异与其水平地带谱相应;亚高山草甸土和灰褐土的氧化还原状况随山体高度和植物群落而呈垂直分异趋势。

Therefore, it is clear that the moisture regime is the principle factor for the land cover change in subhumid and semiarid areas of the mid-temperature zone.

定量计算表明,人类活动所导致的生态破坏在内蒙古奈曼旗50~70年代和50~90年代累计发生的土地沙漠化中所起的作用分别占38.4%和46.7%。

The study area, served as a key part of the subhumid and semiarid areas of midtemperate zone in China, is characterized by the vulnerable eco-environment and most sensitive to global environmental change.

研究工作所涉及的范围是中国中温带半湿润—半干旱区的重要组成部分。

But the change of humid boundaries is not in evidence like the heat boundaries. Before and after 1980, the Subhumid boundary and semiarid boundary move towards west or east by turns.

而干湿界线的变化却不如热量界线变化明显,80年代以前和80年代以后的湿润和半湿润的界线表现为南段东退北段西移。

Modern approach methods of geography, ecology, quantitative analysis, expert integration, remote sensing image analysis and geographical information system were combined to reveal the matters in this paper. The eco-geographical background of the research area and the research work studied by other scholars were comprehensively expatiated. The temporal and spatial variation of precipitation and soil moisture, vegetation and soil distribution, and land use/land cover were compared as well. On the basis of foregoing analysis, the eco-geographical differentiation was discussed. According to principles and indicators, with extension engineering method and integrated analysis, the physical geography boundary between subhumid and semiarid areas were demarcated. By using remote sensing image analysis, wavelet analysis of the perennial precipitation and temperature, and the comparison of temporal and spatial variation of the desertification, this paper accounted for the regional response to global environmental change and suggested the dominant environmental problems.

本文采用了地理学与生态学相结合、定量分析与专家集成相结合、遥感图像解译和地理信息系统相结合的方法,对研究区的生态地理背景和已有研究工作进展情况给予了全面的分析和阐述;通过对区域水分条件(大气降水、土壤水分条件)、植被、土壤、土地利用/土地覆被状况等环境要素的时间与空间特征的对比分析,探讨了研究区内部生态地理特征的差异;在一定的原则指导下,通过建立指标体系,以可拓工程方法和模型为支撑,经过综合分析确定了研究区内半湿润、半干旱区界线划分方案;通过遥感图像解译、典型站点多年降水与温度的小波分析、土地沙漠化时空变化的对比分析等,说明了研究区域对全球变化的响应;表明了该区域所面临的主要环境问题。

Based on the ecological characteristics, climate and humidity condition for the vegetation of the sporopollen from the both of the wells, the palaeovegetation types have been reconstructed. The result shows that the paleoclimate changes from tropical semiarid-subhumid climate to subhumid mid subtropical climate to subhumid south subtropical climate.

通过对两口钻井的孢粉植被类型、气温带和干湿度类型及孢粉谱的进一步分析,可将泉头组-青山口组沉积期的气候变化划分为三个演化阶段,自下向上依次为半干半湿的热带气候——半湿润的中亚热带气候——半湿润的南亚热带气候。

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