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EREE distribution of the surface sediments in Chukchi Sea, high-values are mainly located in the southwest area adjacent to the west and north of Point Barrow area, a significant low in the area of Central. DREE distribution of surface sediments in Bering Sea, the central REE values area higher than that two sides.

楚科奇海表层沉积物中∑REE的分布,高值区主要分布在海区西南侧、西侧和巴罗角以北海域,低值区重要分布在海区中部;白令海表层沉积物中∑REE的分布,南北两侧较中部采样站位值低。

EREE distribution of the su***ce sediments in Chukchi Sea, high-values are mainly located in the southwest area adjacent to the west and north of Point Barrow area, a significant low in the area of Central. DREE distribution of su***ce sediments in Bering Sea, the central REE values area higher than that two sides\'.

楚科奇海表层沉积物中∑REE的分布,高值区主要分布在海区西南侧、西侧和巴罗角以北海域,低值区重要分布在海区中部;白令海表层沉积物中∑REE的分布,南北两侧较中部采样站位值低。

Finally, low pay is mixed between the area the case that the income gap of the unskilled worker appeared to narrow, and hi-tech personnel is mixed between the area the income gap of high quality personnel however incline to at expanding, this part worker's inferior area fluidity and they located labour market was mirrorred to existing on certain level relatively serious area breaks up a gender.

最后,地区之间低报酬和非技术工人的收入差距出现了缩小的情形,而地区之间高技术人员和高素质人员的收入差距却趋向于扩大,在一定程度上反映了这部分职工较低的区域流动性和他们所处的劳动力市场存在着较为严重的地区分割性。

Because of the regional difference of soil and climatic conditions, the division of 4 stages of soil moisture circulation is not all the same between different areas; the soil moisture dynamics between different dry farming areas in the Yellow River Basin is contrasted in this report. The results indicate that soil moisture increases gradually from dry semi-arid area to semi-arid area, dry semi-humid area and semi-humid area, and the high value district generally appears during soil moisture resuming period in rainy season or soil melting period. While the low value district appears at the stage of fast evaporation in spring or slow evaporation in autumn; in views of vertical changes of soil moisture, it is showed that the variation range of upper lays is larger than that of lower among the different dry farming areas in the Yellow River Basin.

由于各区域之间土壤、气候条件的差异,各地土壤水分循环4个阶段的划分也不尽相同;黄河流域不同旱作类型区土壤水分动态变化比较结果表明:就季节变化而言(来源:A70b0B0bC论文网www.abclunwen.com),由半干旱偏旱区→半干旱区→半湿润偏旱区→半湿润区土壤水分含量呈逐渐增加的变化趋势,而且高值区一般出现在雨季恢复阶段或春季土壤融冻返浆时期;而低值区均出现在春季大量蒸发阶段或秋季缓慢蒸发阶段;就垂直变化而言,黄河流域不同旱作类型区土壤水分垂直变化的趋势均表现为上层变化幅度较下层大。

Methods A concept of compartmental localization of heel, including the low area, posterior area, upper area, medial area and lateral area was considered on the base of anatomy, and the difference of soft tissue deepth, compression resistance, confiction resistance, according to which the feeling function was reconstructed by the flaps based on vessel and nerve, or by the flaps based on vessel with nerve anastomasis.

对足跟进行解剖学观察,分别测量各部位软组织厚度,根据各部位承受重力及摩擦程度不同,将跟分为跟底、跟后、跟上、跟内、跟外5个区域。修复时根据各个创面所在区域及软组织厚度不同特点,选择不同的带血管、神经蒂皮瓣或吻合神经的带血管蒂皮瓣转移。

Controlled main faults developed in the area,the studied results of microstructure phenomena reflected the area belong to a deformational environment of shallow crust low temperature,low confining pressure and high strain rate.

通过在野外露头采集定向标本并在室内进行切片研究,对区内主要发育的断裂进行控制,显微构造现象的研究结果反映出本区总体上属于地壳浅层次的低温、低围压和高应变速率的变形环境。

China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,ChinaIt is a difficult task for shadow and feculent water area processing when extracting water body from remote sensing image by traditional methods.Light Laser Detection and Ranging is robust to gain point cloudy data from shadow and feculent water as it has less affection from that area.However,the point cloudy data is always with low resolution which results to contour line with low accuracy.

从遥感影像中提取水体的传统方法在阴影处和水体浑浊处存在一定局限;机载激光雷达获取点云数据时水体受阴影和浑浊的影响小,因此使用点云数据提取水体比使用影像数据更加稳健;但点云数据的分辨率低,所提取的轮廓线精度不高。

When entering the diaphragm pressure on the top of the control room to the atmosphere or water by the downstream area of low pressure, the role of the bottom plate in the valve and the pressure below the diaphragm on the pressure value is greater than the top, so the main valve disc to the fully open position; when entering the diaphragm pressure above the control room can not water the lower reaches of the atmosphere or area of low pressure, the role of the diaphragm on the top of the pressure value is greater than the pressure below the value, so will the main valve pressure valve set to fully closed position; when the diaphragm pressure above the value of the control room at the entrance of the middle pressure and outlet pressure, the main valve in the regulator valve on the disk, and its regulation depends on the location of the needle-catheter system and adjustable valve guide of the role of joint control.

当阀门进入隔膜上方控制室内的压力水被排到大气或下游低压区时,作用在阀盘底部和隔膜下方的压力值就大于上方的压力值,所以将主阀阀盘推到完全开启的位置;当进入隔膜上方控制室内的压力水不能排到大气或下游低压区时,作用在隔膜上方的压力值就大于下方的压力值,所以就会把主阀阀盘压到完全关闭的位置;当隔膜上方控制室内的压力值处于入口压力与出口压力中间时,主阀阀盘就处于调节状态,其调节位置取决于导管系统中的针阀和可调导阀的联合控制作用。

When entering the diaphragm pressure on the top of the control room to the atmosphere or water by the downstream area of low pressure, the role of the bottom plate in the valve and the pressure below the diaphragm on the pressure value is greater than the top, so the main valve disc to the fully open position; when entering the diaphragm pressure above the control room can not water the lower reaches of the atmosphere or area of low pressure, the role of the diaphragm on the top of the pressure value is greater than the pressure below the value, so will the main valve pressure valve set to fully closed position; when the diaphragm pressure above the value of the control room at the entrance of the middle pressure and outlet pressure, the main valve in the regulator valve on the disk, and its regulation depends on the location of the needle-catheter system and adjustable valve guide of the role of joint control.

当进入隔膜上方控制室内的压力水被排到大气或下游低压区时,作用在阀盘底部和隔膜下方的压力值就大于上方的压力值,所以将主阀阀盘推到完全开启的位置;当进入隔膜上方控制室内的压力水不能排到大气或下游低压区时,作用在隔膜上方的压力值就大于下方的压力值,所以就会把主阀阀盘压到完全关闭的位置;当隔膜上方控制室内的压力值处于入口压力与出口压力中间时,主阀阀盘就处于调节状态,其调节位置取决于导管系统中的针阀和可调导阀的联合控制作用。

Results Xunhua-Guide area is characterized by step-shaped low-relief at different elevation. The low-relief surfaces developed above the newer strata in sedimentary basin among the Oligocene to the lower Pleistocene are in higher elevation, but above the older strata, are in lower elevation. The elevations of all above low-relief surfaces are lower than those of the planation surface above the bedrocks in the thrust belts. The low-relief surfaces of terraces, developed on both sides of the deep-cutting valleys within the basins, are lowest in elevation.

结果 循化-贵德地区地形形态总体呈台阶状结构,在不同海拔高度存在低起伏地形;发育于盆地沉积地层之上的低起伏面表现为年代越新的地层之上低起伏面高程越高,越老的地层高程越低,并且它们均低于发育于逆冲带基岩之上的夷平面;发育于盆地深切河谷两侧阶地之上的低起伏面海拔高程总体较低。

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