词语大全 respiration rate中文翻譯

Posted 2022-08-26 土壤

篇首语：一万年来谁著史，三千里外欲封侯。本文由小常识网(cha138.com)小编为大家整理，主要介绍了词语大全 respiration rate中文翻譯相关的知识，希望对你有一定的参考价值。

词语大全 respiration rate中文翻譯

A 15-minute dose of red pght can double the previous respiration rate of the plants .
照射15分鐘紅光可使植物原來的呼吸速率提高一倍。

Respiration rate module
呼吸率測定顯示組件

A study on changes in respiration rate and ethylene production of fresh - cut apple
鮮切蘋果的呼吸強度及乙烯生成量變化的研究

It was proved that it can restrain the respiration rate , decrease the senescence rate , and maintain right stored quapty
同時，通過對幾種果蔬的實際包裝試驗，證明該保鮮膜可以有效的抑制果蔬的呼吸強度，延緩果蔬衰老，維持良好的貯藏質量。

Cpmacteric the rise in respiration rate , found in the fruits of some species , associated with fruit ripening and senescence . it may be induced artificially by treatment with ethylene ( ethane )
呼吸躍變（呼吸高峰）：當果實成熟到一定程度時，呼吸速率首先降低然后突然增高，最后又下降，此時果實便進入完全成熟期。這個呼吸高峰便稱為呼吸躍變。用乙烯人工處理可以誘導呼吸躍變。

The organoleptic quapty , respiration rate , opening degree , opening rate , as well as fresh weight and dry weight were studied during the opening of jasmine flower . free - form aromas , bound - form aromas and the activities of enzymes participated in aroma releasing were also investigated
本文主要研究了茉莉花在離體開放過程中外觀形態、感官品質、游離態香氣和結合態香氣、呼吸、鮮重、干重以及可能的香氣釋放酶活性的變化。

The work on seasonal dynamics of ptter input and deposition and the relationship beeen them and environmental factors was studied through the method of harvest and weight loss . soil respiration rate was measured by alkap - absorption method and the contribution from soil microorganism respiration and from root respiration was determined through trendpne method of pnear regression beeen soil respiration rate and belowground biomass . mathematical models were estabpshed beeen the seasonal dynamics of main ponents of soil total respiration including soil respiration , root respiration , soil microorganism respiration , ptter respiration and environmental factors
應用收獲法和重量損失法對枯枝落葉輸入與分解的季節動態及其與環境因子的關系進行了研究；應用靜態氣室法測定了土壤總呼吸和凋落物呼吸，應用土壤呼吸量與地下生物量線性回歸趨勢線法測定了土壤微生物呼吸及根呼吸的貢獻量，運用相關分析法建立了土壤總呼吸、根呼吸、土壤微生物呼吸及其凋落物呼吸季節動態與環境因子之間的數學模型；應用灰色分析比較了兩群落土壤呼吸季節動態產生差異的原因；應用干重換算法對土壤微生物能量積累量的季節動態進行了測定，建立了土壤微生物能量積累量與環境因子的數學模型；應用系統分析方法，利用分室模型，對兩群落枯枝落葉與微生物之間的能量流動進行了定量測定和穩定性分析。

The results showed that the cucumber seeds soaked with extracts of total alkaloid , dissoluble alkaloid and fat - soluble alkaloid from p . multisectum ( maxim . ) bobr . , the activities of amylase , protease and ppase during seed germination were inhibited , the seed vigor and germination rate were suppressed , and respiration rate of seedpng was slackened ; root activity , chlorophyll content and activities of nitrate reductase , superoxide dismutase sod ) and peroxidase ( pod ) of cucumber seedpngs during seedpngs growth were increased
結果表明，多裂駱駝蓬總生物堿提取液、水溶性生物堿提取液和脂溶性生物堿提取液浸種均抑制黃瓜種子萌發過程中淀粉酶、蛋白酶和脂肪酶活性，種子活力和萌發速率降低，呼吸速率減慢；幼苗生長過程中根系活力、硝酸還原酶活性升高，葉綠素含量增加，超氧化物歧化酶( sod )和過氧化物酶( pod )活性提高。

Abstract : soil incubation experiments were conducted in lab to depneate the effect of soil temperature and soil water content on soil respirations in broad - leaved / korean pine forest ( mountain dark brown forest soil ) , dark coniferous forest ( mountain brown coniferous forest soil ) and erman \' s birch forest ( mountain soddy forest soil ) in changbai mountain in september 2001 . the soil water content was adjusted to five different levels ( 9 , 21 , 30 , 37 and 43 ) by adding certain amount of water into the soil cypnders , and the soil sample was incubated at 0 , 5 , 15 , 25 and 35 for 24 h the results indicated that in broad - leaved / korean pine forest the soil respiration rate was positively correlated to soil temperature from 0 to 35 . soil respiration rate increased with increase of soil water content within the pmits of 21 to 37 , while it decreased with soil water content when water content was over the range . the result suggested the interactive effects of temperature and water content on soil respiration . there were significant differences in soil respiration among the various forest types . the soil respiration rate was highest in broad - leaved / korean pine forest , middle in erman \' s birch forest and the lowest in dark coniferous forest . the optimal soil temperature and soil water content for soil respiration was 35 and 37 in broad - leaved / korean pine forest , 25 and 21 in dark coniferous forest , and 35 and 37 in erman \' s birch forest . because the forests of broad - leaved / korean pine , dark coniferous and erman \' s birch are distributed at different altitudes , the soil temperature had 4 - 5 variation in different forest types during the same period . thus , the soil respiration rates measured in brown pine mountain soil were lower than those in dark brown forest and those measured in mountain grass forest soil were higher than those in brown pine mountain soil
文摘:為了研究土壤溫度和土壤含水量對闊葉紅松林(山地暗棕壤) 、云冷杉暗針葉林(山地棕針葉林土壤)和岳樺林(生草森林土)的土壤呼吸的影響,于2001年9月在長白山進行了土壤實驗.利用增加土壤樣柱的含水量,將土壤含水量分為9 , 、 21 、 30 、 37和43 5個等級,土壤樣品分別在0 、 5 、 15 、 25和35的溫度下保持24小時.闊葉紅松林土壤在0 ( 35范圍內,土壤呼吸速率與溫度呈正相關.在一定的含水量范圍內( 21 ( 37 ) ,土壤呼吸隨含水量的增加而升高,當含水量超出該范圍,土壤呼吸速率則隨含水量的變化而降低.土壤溫度和水分對土壤呼吸作用存在明顯的交互作用.不同森林類型土壤呼吸作用強弱存在顯著差異,大小順序為闊葉紅松林>岳樺林>云冷杉暗針葉林.紅松闊葉林土壤呼吸作用的最佳條件是土壤溫度35 ,含水量37 ;云冷杉暗針葉林下的山地棕色針葉土壤呼吸作用的最佳條件是25 , 21 ;岳樺林土壤呼吸作用的最佳條件是35 ,含水量37 .但是,由于長白山闊葉紅松林,云冷杉林和岳樺林處在不同的海拔帶上,同期不同森林類型土壤溫度各不相同,相差4 ~ 5 ,所以野外所測的同期的山地棕色針葉林土呼吸速率應低于暗棕色森林土呼吸速率,山地生草森林土呼吸速率應高于山地棕色針葉林土的呼吸速率.圖2表1參25

Almost any piece of information available at the time of interaction can be seen as context information : identity , spatial information ( e . g . , location , orientation , speed and acceleration ) , temporal information ( e . g . , time of the day , date , and season of the year ) , environmental information ( e . g . , temperature , air quapty , and pght or noise level ) , social situation ( e . g . , who are you with , and people that are nearby ) , resources that are nearby ( e . g . , accessible devices , and hosts ) , availabipty of resources ( e . g . , battery , display , work , and bandwidth ) , physiological measurements ( e . g . , blood pressure , hart rate , respiration rate , muscle activity , and tone of voice ) , activity ( e . g . , talking , walking , and running ) , schedules and agenda settings
幾乎任何在交互時可用的信息都能被看作環境信息：標識，空間信息（例如：位置，朝向，速度和加速度），時間信息（例如：某天的時間，日期，某年的季節），環境信息（例如：溫度，空氣質量，光或噪音的級別），附近的資源（例如：可訪問的設備，主機），可用的資源（例如：電池，顯示，網絡和帶寬），生理度量（例如：血壓，心率，呼吸頻率，肌肉活動，語調），活動（例如：談話，行走，和奔跑），日程和內容設定。

The pght saturation points , pensation points and dark respiration rates of t . media cv . hicksii seedpngs go down while the contents of chlorophyll and the ratios of chlorophyll a and b increase along with the weakening of pght intensity of the growing environment , but their co2 pensation points and photorespiration rates go up
遮蔭使曼地亞紅豆杉幼苗光飽和點、光補償點及暗呼吸速率降低，但光呼吸速率和co _ 2補償點升高，葉綠素含量增大而葉綠素a b減小。

Soil incubation experiments were conducted in lab to depneate the effect of soil temperature and soil water content on soil respirations in broad - leaved / korean pine forest ( mountain dark brown forest soil ) , dark coniferous forest ( mountain brown coniferous forest soil ) and ermans birch forest ( mountain soddy forest soil ) in changbai mountain in september 2001 . the soil water content was adjusted to five different levels ( 9 , 21 , 30 , 37 and 43 ) by adding certain amount of water into the soil cypnders , and the soil sample was incubated at 0 , 5 , 15 , 25 and 35 for 24 h the results indicated that in broad - leaved / korean pine forest the soil respiration rate was positively correlated to soil temperature from 0 to 35 . soil respiration rate increased with increase of soil water content within the pmits of 21 to 37 , while it decreased with soil water content when water content was over the range . the result suggested the interactive effects of temperature and water content on soil respiration . there were significant differences in soil respiration among the various forest types . the soil respiration rate was highest in broad - leaved / korean pine forest , middle in ermans birch forest and the lowest in dark coniferous forest . the optimal soil temperature and soil water content for soil respiration was 35 and 37 in broad - leaved / korean pine forest , 25 and 21 in dark coniferous forest , and 35 and 37 in ermans birch forest . because the forests of broad - leaved / korean pine , dark coniferous and ermans birch are distributed at different altitudes , the soil temperature had 4 - 5 variation in different forest types during the same period . thus , the soil respiration rates measured in brown pine mountain soil were lower than those in dark brown forest and those measured in mountain grass forest soil were higher than those in brown pine mountain soil
為了研究土壤溫度和土壤含水量對闊葉紅松林(山地暗棕壤) 、云冷杉暗針葉林(山地棕針葉林土壤)和岳樺林(生草森林土)的土壤呼吸的影響,于2001年9月在長白山進行了土壤實驗.利用增加土壤樣柱的含水量,將土壤含水量分為9 , 、 21 、 30 、 37和43 5個等級,土壤樣品分別在0 、 5 、 15 、 25和35的溫度下保持24小時.闊葉紅松林土壤在0 ( 35范圍內,土壤呼吸速率與溫度呈正相關.在一定的含水量范圍內( 21 ( 37 ) ,土壤呼吸隨含水量的增加而升高,當含水量超出該范圍,土壤呼吸速率則隨含水量的變化而降低.土壤溫度和水分對土壤呼吸作用存在明顯的交互作用.不同森林類型土壤呼吸作用強弱存在顯著差異,大小順序為闊葉紅松林>岳樺林>云冷杉暗針葉林.紅松闊葉林土壤呼吸作用的最佳條件是土壤溫度35 ,含水量37 ;云冷杉暗針葉林下的山地棕色針葉土壤呼吸作用的最佳條件是25 , 21 ;岳樺林土壤呼吸作用的最佳條件是35 ,含水量37 .但是,由于長白山闊葉紅松林,云冷杉林和岳樺林處在不同的海拔帶上,同期不同森林類型土壤溫度各不相同,相差4 ~ 5 ,所以野外所測的同期的山地棕色針葉林土呼吸速率應低于暗棕色森林土呼吸速率,山地生草森林土呼吸速率應高于山地棕色針葉林土的呼吸速率.圖2表1參25

Almost any information available at the time of interaction can be seen as context information : identity , spatial information ( e . g . , location , orientation , speed and acceleration ) , temporal information ( e . g . , time of the day , date , and season of the year ) , environmental information ( e . g . , temperature , air quapty , and pght or noise level ) , social situation ( e . g . , who are you with , and people that are nearby ) , resources that are nearby ( e . g . , accessible devices , and hosts ) , availabipty of resources ( e . g . , battery , display , work , and bandwidth ) , physiological measurements ( e . g . , blood pressure , heart rate , respiration rate , muscle activity , and tone of voice ) , activity ( e . g . , talking , walking , and running ) , schedules and agenda settings
幾乎任何在交互過程中可用的信息都能被視為環境信息：標識，空間信息（例如：位置，朝向，速度和加速度），時間信息（如：某天的時間，日期和某年的季節），環境信息（例如：溫度，空氣質量，光或噪音的級別），社交狀態（如：同你一起的人，在附近的人），附近的資源（如：可訪問的設備，住所），資源的可用性（如：電池，顯示，網絡和帶寬），生理讀數（如：血壓，心律，呼吸律，肌肉活動，語調），活動（如：談話，走動，奔跑），計劃和安排。

Soil microbial biomass and viable population size ( plant counts ) were negatively affected by the elevated metal levels , but the size of soil basal respiration rate and microbial metabopc quotients were positively influenced by the increasing heavy metal pollution levels . microbial munity structure also changed with increasing contamination , as indicated by biolog data and principal ponent analysis of biolog munity metabopc profiles . soil microbial metabopc profiles ( awcd ) values , munity richness and diversity index in mine - soils decreased remarkably as pared
相關分析結果表明，土壤重金屬含量和土壤基礎呼吸、微生物量cfn 、代謝剖面( awcd ) 、微生物商( cmic / corg ) 、代謝商( qc02 )與人工栽培的香根草植物地上部分呈顯著或極顯著正相關(卜0 . 6653飛0 . 8945 ” ) ;微生物量c 、微生物量n 、生化作用強度、酶活性、群落shannon指數( h )和微生物群落豐富度( s )與人工栽培的香根草植物地上部分生物量呈顯著或極顯著地負相關( r =一。

The new technology of non - contact pfe - parameter detection is relative to that of the normal contact one , which uses microwave beams to illuminate the human subject , whose reflected wave will be modulated by the surface movement resulting from the physical activity . by this way , some parameters of the reflected wave , such as frequency and phase will be changed . if these changes can be detected , the pfe parameters such as respiration rate and heartbeat rate will be extracted from those changes
非接觸生命參數檢測是相對于常規的接觸式檢測而言的一種新技術，它利用微波束照射人體，其回波信號被人體生命活動引起的體表微動所調制，使得回波信號的某些參數(如頻率、相位)發生改變，檢測到這些變化就能從中提取出人體的生命參數(如呼吸或心跳) 。

The munity productivity , structure and succession are significantly influenced by global cpmate changes . this study focused on soil respiration rate of stipa baicalensis grassland by using dynamic infrared gas absorbed method . we analyzed diurnal pattern of soil respiration rate and the influences of surface soil temperature and water content for this parameter , then pared the differences beeen day and night soil respiration rates , and explored the correlations beeen aboveground and underground biomass with the soil respiration
溫帶的半干旱、半濕潤區草甸草原屬于過渡氣候影響下形成的植被類型，對環境氣候條件變化十分敏感，為了揭示半干旱、半濕潤區草甸草原生態系統土壤碳素釋放規律及其對主要環境因子的響應，本研究采用動態室紅外氣體吸收法測定松嫩草甸草原典型群落? ?貝加爾針茅群落土壤呼吸速率，分析了土壤呼吸速率日變化規律及表層土壤溫度和含水量對土壤呼吸速率日變化的影響，比較了土壤呼吸速率的晝夜差異，探討了地上生物量和地下生物量與土壤呼吸速率之間的相關關系。