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The results showed that compared with soil culture, the root cap was not obvious with less amyloplast and polysaccharose substance under water culture. The root epidermis under water culture was thinner than that of soil culture, with little root hair or not, in which cortex parenchyma tissue developed with big cell, solution proliferative aerenchyma in intercellular space, and thin cell wall. However, the root cap under soil culture was big, with strong PAS reaction and no aerenchyma tissue.

结果表明:水培后根冠不明显,淀粉体较少,多糖类物质较少而土培根根冠体积较大,淀粉体较多,多糖类物质多,土培根PAS反应强烈;水培根表皮厚度比土培根小,水培根根毛少或退化消失;水培根皮层薄壁组织发达,细胞大型,壁薄,细胞间隙中含有溶生性通气组织,土培根皮层未见通气组织。

When big, moderate rain and rainstorm, the Y value size order is always the masson pine pinus elliottii mixed forest<the wetland pinery<the wetland pinery<the locust tree forest<the locust tree pinus elliottii mixed forest<the thin forest, to the soil protection effect, the conifer forest is better than broad leaved forest. For annual rainfall erosion, the Y value ordered: Locust tree forest<wetland pinery<locust tree pinus elliottii mixed forest<wetland pinery<masson pine pinus elliottii mixed forest<thin forest.

大、中雨和暴雨时,Y值的大小顺序都是马尾松湿地松混交林<湿地松林<湿地松林<刺槐林<刺槐湿地松混交林<疏林,对土壤保护效果针叶林优于阔叶林;对于年降雨侵蚀,Y值的大小顺序是:刺槐林<湿地松林<刺槐湿地松混交林<湿地松林<马尾松湿地松混交林<疏林。

This paper explains that the Winkler's model is applicable only to spongy or compressible rather thin soil bed when calculating the sinkage and internal force of the rig-substructure and in general a model of limited compressibility should be used.

本文以计算结果说明计算钻机底座的沉陷和内力时,文克尔模型仅适用于松软的或可压缩的土层较薄的地基,一般情况下应该用有限压缩层模型,这对钻机底座的静力计算有着重要的意义。

This is not surprising, given the closer proximity of Pengyang to the Asian inland dust sources; The average content of calcium carbonateis of Pengyang section is not only higher than that of central loess plateau, but also higher the west of Chinese Loess Plateau, which reflected Pengyang loess had been deposited by near Liupanshan\'s substances that contained more calcium carbonateis; The content of diffluent element of 10m depth in the section increased fast, which indicated that the modern eluviation and the leaching depth of loess may be stronger than our guess; The soil growth index can reflect the intensity of soil forming and the climatic changes; The "abrupt chang" of glacial and interglacial period was caused by strong soil-forming processes that enlarged the discrepancy of granularity between loess and paleosol. However, the magnetic susceptibility nearly cannot reflect the existence of S_8 and the magnetic susceptibility of S_7 is highest in the whole section, which is inconsistent with other studies that S_5 has the highest magnetic susceptibility.Thin-section examination shows that the micro-texture of the soil layers is divided into both cementing texture in S_7, S_5 and S_1, and granular texture in all others.

与其它剖面相比,彭阳剖面粒度总体上要比东部的洛川、西安,甚至西部的兰州、新疆东湾要粗;CaCO_3平均含量不仅高于黄土高原中部,也高于高原西部,反映出本剖面富含碳酸盐的六盘山近源沉积起到了很重要的作用;易溶元素含量在剖面10m处快速升高,淀积特征明显,反映出黄土受现代淋溶成土作用影响较大,黄土直立、疏松、多孔特性和高温与多雨组合的气候特点,使得元素淋溶、淀积的强度和深度超出了传统的认识和判断;烧失量与其它指标相比,不仅能区分冰期、间冰期;而且能够区分出次一级的冰阶、间冰阶,有较高的分辨率;土壤发育指数、红度能够反映土壤强度差异,是反映气候波动的较好指标;然而,磁化率不能反映古土壤S_8的存在,且S_7的磁化率在全剖面中最高,这与大多剖面S_5磁化率最高的特点不一致。4。

The eluvial soils on slopes where surface flow occurs are mainly clayey soils with some blocks or debris. They have good grading distribution and a thin soil horizon.

发生坡面流的斜坡残坡积土主要为粘性土,含少量块石或碎石,级配较好,且土层厚度小。

The thin layer of microbiotic crusts with lower bulk density, lower density, higher soil porosity and higher water-holding capacity will markedly influence the soil hydrological processes, such as the processes of penetration, the interception, the redistribution and the evaporation of precipitation, which will threat the soil-water environment in Shapotou area.

容重较小、比重低、孔隙度高和持水性能强的薄层微生物结皮对土壤水文过程产生了深刻的影响。在沙坡头地区,微生物结皮改变了降雨在沙丘土壤中的渗透、再分配、拦截和蒸发等过程,并最终导致固定沙丘土壤水环境的恶化。

Standard Rico⑿In these great drawing, in that marks is under a dark cloud dim wild thin soil place scenery, roll of thunder lengthened the thin and pale person's shadow totters, is not belongs to mood between this mortal world by one kind to make as if stupefied, they are holding the breath.

格里科⑿的那些伟大的绘画中的一幅,在那幅画上是一片乌云下的昏暗的荒瘠土地的景色,雷声隆隆拖长了的憔悴的人影东歪西倒,被一种不是属于尘世间的情绪弄得恍恍惚惚,他们屏息着。

Contaminants can easily enter the subsurface through thin soil cover in stone forest and via swallow holes at the bottom of depression.

究其原因,尽管药池坝洼地底部土壤层覆盖较厚,但存在地表径流集中排向落水洞,生态石林分布区地表裂隙、溶沟发育,可直接接受雨水入渗,因而污染物极易通过降雨和地表径流过程进入含水层。

The characters of karsts soil are four:(1) soil layer is thin and the soil is barren;(2) the soil is not continuously distribution and separated by the stone-teeth;(3) water and soil resources are separated;(4) slopping field is more, the flat is few.

岩溶区土壤资源的特征是:①成土速率慢,土层薄,土壤贫瘠;②土被不连续,多被石芽所间隔;③水土资源分离;④坡地多、平地少。

I pondered for a long time for the wild apricot write such a poem: in March, your hard Zhigan flashing red / bright flowers, full of festivity Yang / first ray of morning breeze in your Zuiwo Hong Hing / The first round of the Rising Sun will be your rainbow dream sublimation / At this point, you do not calm / dry thin soil slopes of the low-lying land is also very attractive / just because you have scattered red cherry / let loess experienced a glorious wedding / apricot, you have a wild wild long plant / plush velvet acid fruit revealed the life experience of your / you're just waiting for June where Tiantiandixiao the / could be your heart is still sealed so bitter / This is what you do, wild apricot / dedication of the fruit, after the dedication of the nuclear / and you are shaking like that golden leaves / quietly falling.

我思索的久了,为野杏树写下这样一首诗:三月,你坚硬的枝杆闪着红光/耀眼的花朵扬满喜气/第一缕晨风醉卧在你的香馨里/第一轮旭日将你的霓梦升华/此时,你不平静/干廋的土坡洼地也很迷人/只因你散落的红樱/也让黄土经历了一次光彩的婚礼/杏树,你着野生野长的植物/毛绒绒的酸果表露出你的身世/只等六月里你甜甜地笑了/可你密封的心仍是那样苦涩/这就是你吗,野杏树/奉献了果,奉献了核之后/你又是那般摇着金黄的叶子/不声不响地飘落。

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Objective: To study the effect of polycythemia on blood oxygen saturation.

裴蕾目的:观察RBC剧增而引起的高粘血症对血氧饱和度的影响。

Based on SIMPLER algorithm in the curvilinear body-fitted coordinates, the calculations were performed for Pr=0.7, Re=10~1000 on non-orthogonal non-staggered grids which are generated by elliptic equation systems.

采用曲线坐标系下压力与速度耦合的SIMPLER算法,数值研究了周期性渐扩渐缩波纹通道内脉动流动与换热情况,流动Re数的范围为10~1000,Pr数为0.7。

Such a traditional division of the zone of aeration is useful for illustrative purposes.

为了说明的目的,包气带的传统划分是有用的。