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The result shows, grass of Sikkim small hole is temporary decline Yan period with permanent decline water content of Yan period soil is respectively 7.06% be in temporary decline with 6.20%; the Sikkim of Yan period is small after water of Kong Cao answer bibulous and rapid, decline Yan condition is eliminated gradually, appearance of aftertreatment group of answer water 6 H and contrast active of basic consistent;SOD is during threatening processing with markedder than notting have to taking a picture change, the ascendant;CAT that there is certain range after answer water and POD active are in threatening during after rising first, drop, all remarkable prep above contrasts level, and the active;MDA content that still keeps taller after answer water as the extension of time of arid and threatening processing mushroom, to threatening the 8th climate reachs maximum, content of the MDA in the lamina after answer water drops quickly, arrive the 5th day after answer water, content of the MDA in threatening group lamina is adjacent already contrast level.

结果显示,锡金微孔草暂时萎焉期和永久萎焉期土壤含水量分别为7.06%和6.20%;处于暂时萎焉期的锡金微孔草复水后吸水迅速,萎焉状态逐渐消除,复水6 h后处理组外貌和对照基本一致;SOD活性在胁迫处理期间和对照相比无显著变化,复水后有一定幅度的上升;CAT和POD活性在胁迫期间先上升后下降,均显著高于对照水平,且复水后仍然保持较高的活性;MDA含量随着干旱胁迫处理时间的延长而迅速增加,到胁迫第8天时达到最大值,复水后叶片中MDA含量迅速下降,到复水后第5天,胁迫组叶片中MDA含量已接近对照水平。

B using press-volume technique, this paper studied the seasonal changes of water potential at saturated point (Ψ, water potential at turgor loss point (Ψ relative osmotic water content at turgor loss point ROWC(superscript thp, relative water content at turgor loss point RWC(superscript tlp, relative content of apoplastic water, bound water/free water V(subscript a/V, and the difference between (Ψ and (Ψ of Reaurnuria trigyna growing on heavy solonchack, non-salinized soil, and saline soil.

运用压力容积技术,研究了4种盐分生境下长叶红砂饱和含水量时最大渗透势Ψ(上标 sat 下标 s、初始质壁分离时的渗透势Ψ(上标 tlp 下标 s初始质壁分离时渗透水相对含量ROWC(上标 tlp、初始质壁分离时的相对含水量RWC(上标 tlp、质外体水的相对含量、束缚水与自由水的比值V(下标 a/V,以及饱和含水量时最大渗透势与初始质壁分离时的渗透势之差的季节变化。

T the first day after operation, the brain water content was the greatest. Comparison the brain water content of two sides of model group,the side of injection hemoglobin was greater than the anthor side.The brain water content was statistic difference between model group and intervenor groups.But the brain water content of intervenor groups was evidently greater than that of control group .

QP4干预组和HO-1干预组各时间点脑组织含水量明显高于对照组,但不如模型组增高明显;AQP4干预组和HO-1干预组各时间点脑组织含水量与模型组比较均有显著性差异,AQP4干预组与HO-1干预组各时间点脑组织含水量比较差异不明显。

The feasibility of the equipment to measure Tg of amorphous powder is verified with a lot of experimentl results.The Tgs of some typical starches such as corn, pachyrhizus, buckwheat and pea in different water content are obtained by TDA. It is found that the water has plastic effect on starch and the Tg of starch decreases with the increase of water content. Through this study a quantitative expression is established to relate Tg and water content, and it is testified with experimental results for the sticky rice starch with different water content.

采用热膨胀法测定不同含水量下玉米、地瓜、荞麦、豌豆淀粉的玻璃化转变温度,得到了随着含水量的增加Tg降低的关系,探讨了水的增塑作用及影响机理,得到含水量与Tg的定量表达式,并用糯米淀粉的实验值对该关联式的有效性进行了验证,为预测不同含水量的淀粉的玻璃化转变温度及对淀粉的储藏加工提供了理论依据。

Over a 20-year period there was no increase in soil water content in the grazed grassland at depths of 2~9.9 m. There was a small increase(0.5~3.7 mm/a) in soil water content in the protected grassland, however the slow rate of increase suggests that at least 150 years would be needed for ungrazed grassland soils to regain water content similar to that present prior to planting trees. Recharge of deep soil moisture was faster in cropland(15 mm/a), but at this rate it would still take about 40 years to restore cropland soil water content to pre-plantation conditions.

结果表明,人工林死后的放牧荒坡在20a的时间里,其土壤水分没有补偿;人工林死后的保护草地土壤水分有微弱恢复迹象,但年恢复速度在0.5~3.7 mm之间,以这样的速度恢复到持续放牧荒坡的土壤含水量,至少需要150a以上;林后农地土壤含水量有恢复趋势,年平均恢复速度为15 mm左右,其土壤含水量要恢复到持续农地当前的水平,大约需要40a的时间。

Parviflora in shrub communities had the xeromorphic traits in the aspects of ① their secondary xylem had shorter vessel elements, higher vessel frequency, less single porous percentage, lower rays, higher relative conductivity and lower vulnerability index, and ② their leaf had lower water potential, lower water content and free water content, higher bound water content, high ratio of bound to free water content, and less specific leaf area.

扁担木叶片、次生木质部的解剖和水分生理特征均表现出一定的可塑性,其可塑性指数高低顺序为次生木质部解剖特征(0、24)〉水分生理特征(0.19)〉叶片解剖特征(0.18)、与侧柏林和混交林相比,灌丛中扁担木个体对干旱生境有一定的适应能力,表现在次生木质部导管分子短,导管频率高,单孔率低,木纤维短,射线矮小,具有较大的相对输导率和较小的脆性指数;叶片水势、组织含水量、自由水含量较低,叶面积、比叶面积较小,而束缚水含量、束缚水自由水比值较高。

Applied with test of potted plant and measurement absorbency for study physiological response of activity of cell defense enzymes and lipid peroxidation of slash pine's half-sib under water stress. There are 7 families comparison with general slash pine. The contents of superoxide dismutase, catalase, antioxidant, malondialdehyde and the rate of superoxide anion(-O2) generating are mensurated under normal water condition while soil water content is 70% and light water stress while soil water content is 55% to 60% and medium water stress while soil water content is 35% to 40% and heavy water stress while soil water content is 20% to 25%. The test result indicate that either water grads or families of contents of SOD,CAT,AsA,MDA are mighty notable difference. The rate of -O2 generating is notable difference within families. The rate of -O2 generating is mighty notable difference within water grades.

为研究湿地松优良半同胞家系保护酶及脂质过氧化作用对水分逆境的生理响应,采用盆栽试验和吸光度测定结合的方法,以普通湿地松种子为对照,测定了七个湿地松半同胞家系在正常水分状态(土壤相对含水量为70%)、弱度水分胁迫(土壤相对含水量为55%~60%)、中度水分胁迫(土壤相对含水量为35%~40%)和强度水分胁迫(土壤相对含水量为20%~25%)条件下的SOD、CAT、AsA、MDA的含量和-O2产生速率,研究结果表明:无论是不同水分梯度还是不同家系水平,SOD、CAT、AsA活性和MDA含量的差异均达极显著水平,不同家系水平间-O2产生速率有显著差异,不同水分梯度间-O2产生速率差异达极显著水平。

Applied with test of potted plant and measurement absorbency for study response of the contents of photosynthetic pigments of slash pine's half-sib under water stress. There are 7 families comparison with general slash pine. The contents of photosynthetic pigments are mensurated under feebleness water stress while soil water content is 55% to 60% and moderate water stress while soil water content is 35% to 40% and heavy water stress while soil water content is 20% to 25%. The test result indicate that either water grads or families of chlorophyll and chlorophyll a and chlorophyll b and Chla/Chlb and carotenoid and Caro/Chl are mighty notable difference. The Chl and Chla and Chlb and Chla/Chlb little drop from normal soil water to initial water stress. Then drop obvious with increased water stress. The Caro and Caro/Chl little drop firstly from normal soil water to initial water stress,then up in metaphase water stress,after drop in evening water stress. The Chl and Chla and Chlb and Chla/Chlb and Caro of slash pine'half-sib are over general slash pine. The Chl and Chla and Chlb and Chla/Chlb and Caro of 464 and 1027 are over average value of slash pine's half-sib under water stress. The Caro/Chl of 609 and 46 are over average value of slash pine's half-sib under water stress.

为研究湿地松半同胞家系光合色素对水分逆境的响应,采用盆栽试验和吸光度测定方法,以湿地松普通种子为对照,测定了七个湿地松优良半同胞家系在弱度水分胁迫(土壤相对含水量为55%~60%)、中度水分胁迫(土壤相对含水量为35%~40%)和强度水分胁迫(土壤相对含水量为20%~25%)条件下的光合色素,对湿地松优良半同胞家系在不同水分胁迫条件下的光合色素进行了研究,结果表明:无论是不同水分梯度还是不同家系水平,Chl、Chla、Chlb、Chla/Chlb、Caro、Caro/Chl均有极显著差异;从正常水分至水分胁迫初期Chl、Chla、Chlb、Chla/Chlb稍微下降,后随着水分胁迫程度的加深下降较快,从正常水分至水分胁迫初期Caro、Caro/Chl先稍微下降,胁迫中期上升,胁迫后期下降;所有半同胞家系的Chl、Chla、Chlb、Chla/Chlb、Caro高于普通种,在水分胁迫条件下家系464、1027的Chl、Chla、Chlb、Chla/Chlb、Caro高于家系的平均水平,家系609、46的Caro/Chl值高于家系的平均水平。

Based on constant altitude plan data like reflectivity factor, collected by a new weather radar interpolated with 3D-Barnes scheme, in this paper the vertically integrated liquid water content and vertically integrated liquid water content density of hailstone cells are calculated with the theoretical model, ration of VIL and upright height of hailstone cells, and the maximums of VIL and VILD are identified using MAX function.

以3D-Barnes方案插值的新一代天气雷达反射率因子等高平面资料,用垂直累积液态含水量(vertically in-tegrated liquid water content,简称VIL)的理论模式计算单体的VIL,用VIL与单体顶高度之比计算单体的垂直累积液态含水量密度(vertically integrated liquid water content density,简称VILD),利用MAX函数逐个提取雹云单体在降雹过程中的最大VIL和VILD(分别简称VILmax和VILDmax),采用统计和回归处理技术,利用2004-2006年的5~8月甘肃中部54例局地冰雹单体个例,对单体VILmax和VILDmax与地面最大降雹区的位置、地面最大冰雹直径之间的相关性以及对Rmax的识别效果等进行了对比分析。

Saturated soil water content, field water capacity and wilting coefficient of all the three parent material purple soil also reduces from top to bottom in the soil profile, but effective water content increases from top to bottom in the soil profile except the layer B of J_(3S). The result of saturated soil water content, field water capacity and wilting coefficient is J_(3P)>J_(2S)>J_(3S), and the result of effective water content is J_(2S)>J_(3P)>J_(3S).

而有效水含量除遂宁组B层外,在剖面呈自上而下的递增趋势,其中田间持水量、萎蔫系数表现为蓬莱镇组>沙溪庙组>遂宁组,有效水含量表现为沙溪庙组>蓬莱镇组>遂宁组。

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