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The soil potential is in accordance with the pondage stage the variety mutually, The soil potential of the current total from diminish to back up again greatly, just the soil layer is from the top bottom, the water potential of the current value enlarge, the water potential changes to let up, the 100 cm soil layer is as follows almost yearly stable.

土壤水势变化与贮水量三阶段相对应,总体由大变小再回升,只是土壤剖面空间从上而下,水势值增大,变幅减小,100cm土层以下近乎常年稳定。

The recovery rate of RN was significantly positive related to root length density and root dry weight in corresponding layers.

玉米和茄子对土壤剖面不同位置累积硝态氮利用率的高低,不仅与作物吸氮量有关,而且与作物的根系分布有关。

In order to obtain good converted wave signals, primary wavefield investigation is required for designing the seismic configuration parameters.

鉴于结晶岩地区波场的复杂性,在剖面调查之前要先进行波场特征调查,才能确定三分量地震调查观测系统采集参数。

On the basis of pollen analysis of surface sample in North China, polynomial function analysis method was applied to establish pollen climate response surface of Pinus, Betula, Quercus, Artemisia, Chenopodiaceae, Compositae, Picea, Ephedra, Gramineae in North China, therefore an easy and applicable method for reconstructing palaeoclimate and palaeoenvironment with data of fossil pollen was founded; Multi-analysis method was applied to analyse the principal elements of surface sample pollen in central Inner Mongolia Steppe, the assemblages of surface sample pollen in steppe area and its relationship with vegetation type were discussed with helps from spore-pollen analysis of a peat section in Chasuqi, Inner Mongolia and 〓C chronometer, fossil pollen data were obtained with high resolution on the peat section in Chasuqi. Vegetation succession and environmental changes since Holocene at resolution of 70 years were primarily reconstructed in south Mount Daqingshan and Plain Tumete. The changes in the area were copmared with those in the neighbouring areas during the same period. It was found that Holocene environmental change had undergone the following stages: cold-arid, temperate-wet, warm-wet, temperate-arid and cold-arid, and the climatical optimum period occurred in 5000-4100 aB.

本文在对中国北方表土花粉研究的基础上,采用多项式函数回归方法建造了中国北方松属、桦属、栎属、蒿属、藜科、菊科、云杉属、麻黄属、禾本科等的花粉——气候趋势面,从而为利用化石花粉资料直接恢复古气候、古环境提供了一种方便易行的方法;采用多元分析方法对内蒙古中部草原区表土花粉进行了主成分分析,探讨了草原区表土花粉组合的规律及与植被类型的关系;本文还应用孢粉分析方法,结合〓C测年技术,通过内蒙古中部察素齐泥炭剖面高分辨率的化石花粉数据,初步恢复了大青山山地南部及土默特平原地区分辨率为70年的全新世以来植被演替和环境变迁的状况,并与邻近地区的全新世古气候、古环境进行了对比研究,研究发现,本区域全新世古环境的变迁序列基本上可以与周围地区及华北地区进行对比,其环境变迁经历了凉干~温湿~暖湿~温干~凉干的变化,且气候最适宜期出现在5000~4100aB.P。

The aim of this research is to finish design of a towed system of 200m depth profiling.

研究目标是设计完成200m深度剖面的拖曳系统。

Turbulent flow about a 4:1 prolate spheroid was measured on cross sections using the PIV technique for validating turbulence models.

为了检验湍流模型,用PIV方法测量了绕4:1椭球湍流流场的几个剖面

The thickness of Yangzhuang Formation is small compared with the whole Proterozoic section , but it has multiple types of rocks with special origins.

杨庄组在整个中、新元古界剖面中厚度不大,但其岩石类型多样且成因特殊。

Two chloride profiles of unsaturated zone at piedmont plain of Taihang Mountains suggestedthat there are three climatic cycles showing the cold-dry or wet-warm conditions over the psat 300years.

太行山前的两个包气带剖面氯含量变化记录说明:过去300年来该区古气候存在三次干湿变化旋回,湿期分别是公元1702-1725年,1761-1825年,1876-1892年。

Oceanic lithospheric mantle harzburgite occurs together with meta-cumulate complex (including garnet pyroxenite and kyanite-eclogite) and MORB-related eclogite; these represent blocks of oceanic lithosphere.

2大洋蛇绿岩型地幔橄榄岩,与变质的堆晶杂岩(包括石榴辉石岩、蓝晶石榴辉岩)和具有大洋玄武岩特征的榴辉岩构成典型的蛇绿岩剖面,代表大洋岩石圈残片。

Oceanic lithospheric mantle harzburgite occurs together with meta-cumulate complex (including garnet pyroxenite and kyanite-eclogite) and MORE-related eclogite; these represent blocks of oceanic lithosphere.

2大洋蛇绿岩型地幔橄榄岩,与变质的堆晶杂岩(包括石榴辉石岩、蓝晶石榴辉岩)和具有大洋玄武岩特征的榴辉岩构成典型的蛇绿岩剖面,代表大洋岩石圈残片。

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