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Multiple wavelengths characteristics of dayside aurora activities were investigated with these keograms and in reference to all-sky images. It was found that there are three repeatedly appearing aurora activity regions along the dayside aurora oval. They are, Region A around 0900MLT in which aurora moves poleward while its intensity decreasing, and its form changingfrom arc to corona with time; Region B around 1330MLT in which aurora moves equatorward while its intensity increasing, and its form changing from corona to arc in time; Region C around 1330MLT in which aurora expands poleward while its intensity decreasing, and its forma evolving from arc to multiple arcs in time. There is a narrow belt of aurora activity in North-South direction between Regions A and B, which is dominated by weak and red corona aurora.

初步分析发现,沿日侧极光卵不论磁静日还是磁扰日,在三个波段上都同时观测到了四个重复出现的极光活动区,即0900MLT附近的A区、1330MLT的B区和1630MLT的C区以及1200MLT附近的G区。A区内的极光活动由低纬高纬运动,强度逐渐变弱,形态由较宽的弧状极光冕状极光演变;B区内的极光活动由高纬低纬方运动,形态呈现为冕状极光较窄的极光弧的演变,极光强度逐渐增强;C区极光活动高纬方展宽,强度逐渐变弱,极光由单弧多重弧演化;而在A与B之间存在一个纬度范围相对较窄的极光活动区G区,该区的极光呈现暗弱的冕状极光。

Simulation experiment and cases shows that change in seal space(both cross sectionally and areally) causes spatial variety of vertical seal in a same fault(both cross sectionally and areally).

通过模拟实验和实例对断层垂封闭的差异性进行了研究,表明由于封闭空间变化造成同一条断层垂封闭性在空间上存在着差异性,由于封闭条件和机理演化造成同一条断层垂封闭在时间上存在着差异性,由于封闭对象改变造成同一条断层垂封闭能力存在着差异性,在相同条件下,同一条断层垂封油能力强于垂封气能力。

"Gotami, the qualities of which you may know,'These qualities lead to dispassion, not to passion; to being unfettered and not to being fettered; to self-effacement and not to self-aggrandizement; to modesty and not to ambition; to contentment and not to discontent; to seclusion and not to entanglement; to energy and not to idleness; to being unburdensome and not to being burdensome': You may definitely hold,'This is the Dhamma, this is the Vinaya, this is the Teacher's instruction.'"

Gotami,这些你所知道的法的特质,'这些法引导清净,不是热情;是往解脱,而不是往束缚;是能抹去自我的贡高,而不是朝自我的贡高;朝歉虚,而不是朝野心;朝满足,而不是不知足;朝独自的闲居,而不是人们的缠缚;精力,而不是懒惰;无烦恼,而不是烦恼':你就可以知道,'这就是经法,这就是戒律,这就是导师的指导'。

"Gotami, the qualities of which you may know,'These qualities lead todispassion, not to passion; to being unfettered and not to beingfettered; to self-effacement and not to self-aggrandizement; to modestyand not to ambition; to contentment and not to discontent; to seclusionand not to entanglement; to energy and not to idleness; to beingunburdensome and not to being burdensome': You may definitely hold,'This is the Dhamma, this is the Vinaya, this is the Teacher'sinstruction.'"

Gotami,这些你所知道的法的特质,'这些法引导清净,不是热情;是往解脱,而不是往束缚;是能抹去自我的贡高,而不是朝自我的贡高;朝歉虚,而不是朝野心;朝满足,而不是不知足;朝独自的闲居,而不是人们的缠缚;精力,而不是懒惰;无烦恼,而不是烦恼':你就可以知道,'这就是经法,这就是戒律,这就是导师的指导'。

Thence in a southeasterly direction to Corner Point No. CP14 (X = 484 330, Y = 683 415); thence in a. northeasterly direction to Corner Point No. CP15 (X = 484 390, Y = 683 490); thence in a southeasterly direction to Corner Point No. CP16 (X = 484 415, Y = 683 470); thence in a southwesterly direction to Corner Point No. CP17 (X = 484 355, Y = 683 395); thence in a southeasterly direction to Corner Point No. CP18 (X = 484 430, Y = 683 335); thence in a southeasterly direction to Corner Point No. CP1, the point of beginning.

从该点起东南延伸至隅角点CP14(X = 484 330,Y = 683 415);从该点起东北延伸至隅角点CP15(X = 484 390,Y = 683 490);从该点起东南延伸至隅角点CP16(X = 484 415,Y = 683 470);从该点起西南延伸至隅角点CP17(X = 484 355,Y = 683 395);从该点起东南延伸至隅角点CP18(X = 484 430,Y = 683 335);从该点起东南延伸至隅角点CP1。

Living office at there face there is existed in new leaf to doing correction being of zero send the centre heart court oneself a to be made move round by strike there existing in some nature what climax holds stock right office middle in Yan quilt in attaching oneself to there to being worth paying attention to holding out to go on pay court to existence there deliver letter all kinds of degree face recipient strike existence strike neighbouring there hold office at court faction part at the head

居住办公室阿特那里朝那里存在被存在在朝派新树叶干的事改正存在的作归零校正送信居中心脏求爱自己a被制做移动变圆了在附近打击那里存在在朝派一些本质什么达到高潮着力点股票权利办公室中部在朝派Yan缝被在朝派附属自己那里存在价值值得注意支持住在野派剩下的右手击球员的左后方场地值得求爱存在那里履行刻印刷体字母各种各样的度朝受主打击存在打击邻近的那里支持住办公室阿特求爱派别分开阿特头儿

Sympegma regelii community, a rangeland desert vegetation, has the highest Shannon-Winner species diversity indices (1.706); the communities of Haloxylon ammodendron and Ephedra przewalskii, which have obvious feature of desert vegetation, are in the middle in species diversity indices (0.875-0.890); the communities of Calligonum mongolicum, Populus euphratica, Tamarix ramosissima and Glycyrrhiza inflata, characterized by desert forest of which saline desert bushes and saline meadows are scattered in the communities, have lowest value of the species diversity indices (0.079-0.495). 3 The structure of desert plant community is dominated by the bush layer. The species diversity indices of bush layer (0.769-1.451) is much higher than that of herb layer (0.193-0.254), and the diversity in herb layer is strongly influenced by bush layer. 4 The species diversity of desert plant communities shows a gradient of change with respect to longitude, latitude and elevation. For example, rangeland plant Sympegma regelii, with a high level of diversity indices (1.706), is in transition to desert plants Haloxylon ammodendronn community (with a low level of diversity indices of 1.379) in a longitude gradient and to saline Tamarix ramosessima community (with a low level of diversity indices of 0.376) in a latitude gradient. Calligonum mongolicum community, with a low level of species diversity (0.819), is in transition to Ephedra przewalskii (with a low level of diversity indices of 0.890) and Haloxylon ammondendron community (with the diversity indices of 0.645) in an elevational gradient.

群落Shannon-Wiener物种多样性水平表现为合头草群落最高(1.706),具有草原化荒漠植被类型的成分;梭梭群落、膜果麻黄群落居中(0.875~0.890),荒漠植被类型特征明显;沙拐枣群落、胡杨群落、多枝柽柳群落、胀果甘草群落较低(0.079~0.495),荒漠林、盐地沙生灌丛及盐化草甸植被均有零星分布。3荒漠植物群落结构层次中,灌木层占居主导地位,群落灌木层物种多样性水平(0.769~1.451)远远大于草本层(0.193~0.254),且草本层物种多样性受灌木层影响较大。4荒漠植物群落物种多样性分布格局表现为经、纬和海拔梯度的变化,经、纬变化为物种多样性水平较高的草原化植物合头草群落(1.076)物种多样性水平较低的荒漠植物梭梭群落(1.379)和盐化植物多枝柽柳群落(0.376)的过渡,海拔梯度则呈现低水平的沙拐枣群落(0.819)到高水平的膜果麻黄群落(0.890)低水平的梭梭群落(0.645)变化。

After being loaded with horizontal retraction force at various height, displacement and stress distribution of anterior teeth was not well-distributed. Labiolingual displacement of incisors varied from crown lingual tipping to lingual translation and lingual controlling root movement, while canine mainly showed crown lingual tipping. The displacements of teeth increased with the length of hook but their moving tendency remained unchanged. Stress distribution in PDL was in accordance with teeth displacement.

2水平后牵引力的作用点升高时,上前牙的位移和应力分布趋势各不相同:切牙的唇舌位移由冠舌倾斜逐渐变为舌整体移动和舌控根移动,尖牙则以冠舌倾斜位移为主;前牙位移量随牵引力高度增加而增大,但位移趋势较为稳定;牙周膜应力分布与其位移趋势相一致。

Settlement characteristics are studied based on formula of suspended sediment settling velocity and previous research results. Results show that the suspended sediment flux quickly decreases from the Hangzhou Bay to the offshore area. Although the suspended sediments are primarily transported towards the offshore area, net transport towards the Hangzhou Bay is also found in the study area. The study area is basically located in hydrodynamic balance belt, and the suspended sediment transport is characteristics of reciprocating movement and small amount of net sediment discharge. The net suspended sediment transport is mainly controlled by average current transport, Stokes drift-induced transport and gravitational circulation transport. The advection transport effect gradually weakens and gravitational circulation transport evidently intensifies from Hangzhou Bay to the offshore area. Settling velocity of single particles is far smaller than that of floccules, so, influence of flocculation of suspended sediments must be taken into the consideration.

结果表明,研究区净悬沙通量自杭州湾内外海迅速变小,悬沙总体由杭州湾外海输运,但同时存在杭州湾方的净输沙;研究区基本处于水动力平衡带,悬沙输运具有往复搬运、净输沙量小的特点;平均流输运、Stokes漂移输运和垂净环流输运是引起悬沙泥沙净输运的主要作用机制,自口门至外海,平流输运作用逐渐减弱,垂净环流输沙在悬沙净输运中所占比例逐渐增加;舟山群岛海域既是杭州湾东海输运泥沙的重要通道,也是东海沿岸流携带泥沙南输运的过渡地带;研究区单颗粒泥沙沉降速度很小,远小于絮凝沉降速度,在研究本区悬沙沉降时必须考虑絮凝的影响。

The study area is basically located in hydrodynamic balance belt, and the suspended sediment transport is characteristics of reciprocating movement and small amount of net sediment discharge. The net suspended sediment transport is mainly controlled by average current transport, Stokes drift-induced transport and gravitational circulation transport. The advection transport effect gradually weakens and gravitational circulation transport evidently intensifies from Hangzhou Bay to the offshore area. Settling velocity of single particles is far smaller than that of floccules, so, influence of flocculation of suspended sediments must be taken into the consideration.Incipient velocity and transport flux of surface sediments are analyzed using formulas of incipient velocity and transport flux. Transport trend and controlling factors of surface sediments are studied by the method of grain size trend analysis.

结果表明,研究区净悬沙通量自杭州湾内外海迅速变小,悬沙总体由杭州湾外海输运,但同时存在杭州湾方的净输沙;研究区基本处于水动力平衡带,悬沙输运具有往复搬运、净输沙量小的特点;平均流输运、Stokes漂移输运和垂净环流输运是引起悬沙泥沙净输运的主要作用机制,自口门至外海,平流输运作用逐渐减弱,垂净环流输沙在悬沙净输运中所占比例逐渐增加;舟山群岛海域既是杭州湾东海输运泥沙的重要通道,也是东海沿岸流携带泥沙南输运的过渡地带;研究区单颗粒泥沙沉降速度很小,远小于絮凝沉降速度,在研究本区悬沙沉降时必须考虑絮凝的影响。

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