最低持水量 的英文怎麼說

中文拼音 [zuìchíshuǐliáng]
最低持水量 英文
minimum water capacity
  • : 副詞(表示某種屬性超過所有同類的人或事物) most; best; worst; first; very; least; above all; -est
  • : 動詞1 (拿著; 握著) hold; grasp 2 (持有; 保持) keep; hold 3 (支持; 保持) support; maintain 4...
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • : 量動1. (度量) measure 2. (估量) estimate; size up
  • 水量 : water yield; the yield of water水量計[表] watermeter; 水量平衡 water balance; 水量收支 water budget
  1. By investigation on the relationship between period, quantity, extend of ostrinia furnacalis emergence and meteorological factors in qiqihaer, this paper analyzes the factors which effect on period, quantity, extend of ostrinia furnacalis about annual wave. the beginning time of ostrinia furnacalis pupae emergence depends on average temperature in may and june, weather conditions in july decide whether ostrinia furnacalis pupae finish ahead of time ; the beginning time of eclosion is decided by average lowest temperature and precipitation in may and june, and the end time of eclosion is decided by average lowest temperature in june and july, meantime, the length of time of ostrinia furnacalis eclosion and time of grub emergence influence on the extent of ostrinia furnacalis. an important condition of a great emergence of ostrinia furnacalis is that how temperature matchs humidity, which substantially result in reduction of maize output

    本研究項目通過對齊齊哈爾市玉米螟發生期、發生、發生程度與氣象條件關系的分析,找出玉米螟發生期、發生、發生程度年際波動的影響因子: 5 、 6月的平均氣溫決定了玉米螟化蛹開始的早晚, 7月的天氣條件決定玉米螟化蛹是否提前結束; 5 、 6月的平均氣溫和降則決定羽化開始的早晚, 6 、 7月的平均氣溫又決定了玉米螟羽化結束的早晚;而玉米螟羽化續時間的長短和幼蟲發生的早晚影響了玉米螟的發生程度;溫濕條件配合適當與否是促使玉米螟大發生的重要條件,玉米螟大發生又會引起玉米的大幅度減產。
  2. Abstract : soil incubation experiments were conducted in lab to delineate 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 cylinders, 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 limits 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對闊葉紅松林(山地暗棕壤) 、雲冷杉暗針葉林(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,於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,將土壤含分為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.在一定的含范圍內( 21 ( 37 ) ,土壤呼吸隨含的增加而升高,當含超出該范圍,土壤呼吸速率則隨含的變化而降.土壤溫度和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>雲冷杉暗針葉林.紅松闊葉林土壤呼吸作用的佳條件是土壤溫度35 ,含37 ;雲冷杉暗針葉林下的山地棕色針葉土壤呼吸作用的佳條件是25 , 21 ;岳樺林土壤呼吸作用的佳條件是35 ,含37 .但是,由於長白山闊葉紅松林,雲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於暗棕色森林土呼吸速率,山地生草森林土呼吸速率應高於山地棕色針葉林土的呼吸速率.圖2表1參25
  3. Soil incubation experiments were conducted in lab to delineate 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 cylinders, 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 limits 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對闊葉紅松林(山地暗棕壤) 、雲冷杉暗針葉林(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,於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,將土壤含分為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.在一定的含范圍內( 21 ( 37 ) ,土壤呼吸隨含的增加而升高,當含超出該范圍,土壤呼吸速率則隨含的變化而降.土壤溫度和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>雲冷杉暗針葉林.紅松闊葉林土壤呼吸作用的佳條件是土壤溫度35 ,含37 ;雲冷杉暗針葉林下的山地棕色針葉土壤呼吸作用的佳條件是25 , 21 ;岳樺林土壤呼吸作用的佳條件是35 ,含37 .但是,由於長白山闊葉紅松林,雲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於暗棕色森林土呼吸速率,山地生草森林土呼吸速率應高於山地棕色針葉林土的呼吸速率.圖2表1參25
  4. As the dmso concentration ( wt / wt ) in the second coagulation bam increases, the water flux and the clearance rates of urea and creatintine first decrease men keep in a relatively low level and increase at last

    隨著第二凝固浴dmso濃度( wt / wt )的增加,和肌肝、尿素去除率均是先下降,然後保在較平,後又呈上升的趨勢。
  5. In ported trials, wu gave the minimum tr of all plants, and its diurnal maximum tr persisted stability the most within the range of soil moisture 20. 4 % - 6. 4 %. ; nx lowered its tr and shrank its high - low lines after had experienced irregular wet - drought hardening period during culturing ; kerqin performed a plasticity as compared to field ; c. lanata also stood the most stability but on the basis of middle - high maximum tr level ; tr by caragana korshinski was high when soil water was abundant, but was lowest for lack of water ( 6. 4 % )

    盆栽試驗表明,華北駝絨藜蒸騰弱,且在土壤含20 . 4 6 . 4的范圍內高蒸騰速率穩定性強;經脅迫鍛煉寧夏駝絨藜蒸騰降,變幅減小;科爾沁駝絨藜與大田相比蒸騰可塑性較強;土壤分變化中,北美駝絨藜蒸騰在中高平上維穩定的能力強;分良好時檸條蒸騰很強,分脅迫中蒸騰極大降
  6. During this time both the monthly average algae density and lasting time increased year after year. the main algae forming algae bloom was cyanophyta and the dominant generas were microcystis. the accumulation of nutrients ( such as total nitrogen and total phosphorus ) with high concentration, high temperature of water and strong sunshine caused the algae bloom

    結果表明,溫較高的夏秋季(一般為7 9月)是天津市城市供源的藻類高發期;近幾年,高藻期含藻呈逐年增加趨勢,續時間呈逐年延長趨勢;高藻期以藍藻為主,所佔藻類總數高和比例分別為91和70 ,其中的優勢屬為微囊藻屬;中高含的氮、磷等營養鹽是藻類高發的內在因素,溫、光照等是外在誘發因素。
  7. Longgang nature reserve plays an important role in preserving two langur species of both white - headed langur and francois langur. interview and field survey methods were used to survey the distribution and population size of these two langurs in this natural reserve from december 2001 to january 2002. the result indicated that the reserve has 8 groups of white - headed langur with 68 individuals in longrui and 10 groups of francois langur with 75 individuals in longgang. the distribution area and population size of both of the two langurs in this reserve have greatly declined in the past decades. they are seriously threatened and have high risk of disappearance from this reserve if no effective measures are to be taken at once

    為了確定弄崗自然保護區內白頭葉猴的種群數,彌補黑葉猴種群數的空白,掌握此保護區葉猴的生存現狀,採用訪問法和實地數統計法相結合的方法對弄崗自然保護區的弄崗、隴瑞和弄呼3個部分進行深入的調查研究.調查結果表明,在隴瑞片范圍內,共有8群白頭葉猴,種群大小在68隻左右,和20世紀80年代末的244隻相比,數下降相當驚人;在弄崗片內,共記錄到黑葉猴群10群,大的種群為11隻個體,小的種群是4隻個體,共計約有75隻黑葉猴(絕對數統計) ;弄呼的黑葉猴種群已經于上個世紀的晚期消失.造成目前狀況的因素主要是過度狩獵和其他形式的過度干擾.弄崗自然保護區的葉猴種群數已經接近可續繁殖種群的平,如不採取有效的保護措施,這個種群將很可能在短期內消失
  8. Using plots with water and fertilizer fully controlled, the effect of photosynthetic characteristic and yield under different treatments of water and fertilizer coupling was investigated. the result showed that photosynthetic rates are different among treatments of water and fertilizer coupling, and the change of stomatal conductivity is the same as photosynthetic rat. there is almost no influence on evaporation rate and cellular co2 concentration the combination of fertilizer and manure under natural rainfall is beneficial to the maintenance of photosynthetic rate during grain filling, thus results in highter yield and good quality. however, the coupling of fertilizer and manure with sufficient water results in the decline of photosynthetic rate and stomatal conductivity, the yield decreased indicating there has a balance ratio between water and nutrients ( fertilizer and manure ) supply. the study proposed that the optimum management to exploring yield and qlality potential is the combination of fertilizer and manure application with no irrigation

    利用可精確控制分條件的肥平衡場,在不同肥耦合處理的條件下,研究了肥耦合對玉米光合特性及產的影響,結果表明:不同肥耦合處理的條件下,玉米的光合速率有所不同,氣孔導度的變化與光合速率的變化表現基本一致,而對蒸騰速率、細胞間co2濃度影響不大.其中,在自然降條件下,有機肥和無機肥的配合,有利於玉米子粒灌漿期維較高的光合速率,表現出良好的產潛力.充足條件下,有機肥和無機肥的配合,光合速率及氣孔導度表現較,表現產有所下降,說明供與施肥之間有一個平衡系數.表明黑龍江省北部黑土區自然生態條件下,為充分發揮玉米的產潛力,佳的管理措施是增施無機肥和有機肥的配合
  9. Therefor whenever the flood was coming, it is very important that we were prepared to control flood at any moment and safeguard our lives and property and did our best to minimized the damage by some science means, the dss of controlling the flood this paper introduced ought to reflect flood disaster real - timely, list all feasible projects by referring to historic experiences and pre - making plans, find out the optimization of all projects by integrated evaluating for decision maker

    因此,當洪到來時,作好防洪準備,採取有效措施,隨時保護人民的生命財產的安全,盡把損失降程度,意義十分重大。防洪決策支系統的建立,必須能為決策者展現洪災實時的具體情況,參照歷史經驗和預先制定的防洪預案,列出適合當前洪狀態的全部防洪方案可行集,利用綜合評價方法求出洪災損失小的優防洪方案。
  10. N sources ( including organic and inorganic n tested ) and c sources tested could restrain methane oxidation. cellulose inhibited methane oxidation most weakly while the high concentration of methanol and glucose did dramatically, but the proper concentration of methanol could stimulate soil methane oxidation sharply. in the middle process of methane oxidation, addition of glucose could restrain methane oxidation shortly but the inhibition could be relieved about 5 days later when supplied again with enough oxygen

    土壤微生物是甲烷氧化的主要生物類群,含對土壤甲烷氧化活性有明顯影響,過高或過對甲烷氧化均具有抑制作用;氮源(包括有機和無機氮源)對甲烷氧化均有抑制作用;不同碳源對甲烷氧化的影響各異,纖維素對甲烷氧化抑制作用小,而高濃度的甲醇、葡萄糖則對甲烷氧化具有強烈抑制作用;而適當濃度的甲醇可極大促進土壤對甲烷的氧化:在甲烷氧化過程中加入葡萄糖能迅速抑制甲烷氧化;在加入葡萄糖的同時保瓶中充足的氧氣,則這種抑制作用可以在重新培養一定時間后得到解除。
  11. Soil saturated capacity, capillary capacity, total porosity and capillary porosity showed the trend of the " u " during the successional course of artificial forest, namely, they reduced on the early successional stages, after picea reached mature forest, soil porosity recovered slowly. the content of natural water was mainly affected by capillary porosity. from soil chemical properties analysis, the content of soil organic, humus, ha, fa and ha / fa of topsoil was more than that of bottom layer

    即人工雲杉幼林向成熟林演替階段,土壤飽和、毛管及總孔隙和毛管孔隙則減少,在40年生雲杉林達值,之後隨著雲杉自疏,微生態改善,林地凋落物分解加快,土壤飽和、毛管及總孔隙和毛管孔有上升的趨勢,毛管是決定林地自然含的主要因子。
  12. With a powerful and professional researching and exploiting team, keep the pace with the international advanced solar water heater product line, insure the excellent quality of the hinon ' s product, at the same time, picking the australia sydney university ss - c / cu plating technique of selective complex absorption coat, both the product performances and the technique indexes have reached the international advanced level

    依託英國集團總部雄厚的技術力,與國內多所工程設計研究院建立廣泛合作平臺的優勢,喜能公司一直致力於成為方案解決中心,公司的專業技術顧問將為您提供全面卓越的優化技術和方法,通過方案中心長期的技術積累,能夠以優的用方案幫助客戶實現的運營成本,讓客戶從技術優勢中獲取大經濟效益。
  13. The reduced minimum cement contents shall only be used when trial mixes have verified that concrete with a maximum free water / cement ratio not greater than that given for a particular condition can be consistently produced and it is suitable for the conditions of placing and compacting

    只有經過試拌證實,可以續不斷地生產出灰比不大於某一特定工況給定值的混凝土,而且這種混凝土適合於攤鋪與夯實,在這種情況下,才可以使用這一縮減的泥用
  14. Chlorophyll and carotenoid content were lowest. anthocyanin accumulaing slower before the fruits were harvested, chlorophyll and carotenoid content increased. as anthocyanin of red currant fruits, chlorophyll and carotenoid content continuous decreased ; chlorophyll and carotenoid content of white currant fruits uninterrupted reduced during the middle and late stage of development, but anthocyanin content was extreme little

    黑穗醋栗果實花青苷迅速積累期,葉綠素和類胡蘿卜素含處于平,採收前花青苷積累緩慢,葉綠素和類胡蘿卜素含增加;紅穗醋栗果實花青苷積累,葉綠素和類胡蘿卜素含不斷減少;白穗醋栗果實葉綠素和類胡蘿卜素含在中後期續下降,而花青苷積累極少。
  15. General : this device can be mounted on wall, and producing the distil water in lower cost, continuously, automatically and effectively

    概述:該裝置可安裝于墻上,設計為以的經濟成本續、自動、有效地生產高質的蒸餾
  16. The correlation coefficients between soil moisture regime and soil n2o emission rate were positive in the lower soil moisture regime ( 8 to 58 percent wfps ), and soil n2o emission rate turned weaker and weaker when above the field moisture capacity ( 106 percent wfps ). the highest n2o emission rate occurred in the field moisture capacity. soil n2o emission rate was higher in 30 than in 10 in the lower soil moisture regime ( 8 to 58 percent wfps ), however, the trend was reverse when above the field moisture capacity ( 106 percent wfps )

    5分含時( 8 58 wfps ) ,土壤中n20釋放速率與土壤濕度呈正相關,並且隨著溫度升高釋放速率增大;土壤濕度接近田間( 58 wfps )時,釋放速率大;超過田間( 106 wfps )時, n _ 2o釋放速率顯著降,且30時的釋放速率小於10時的速率。
  17. The results were as follows : 1. on the basis of saline water infiltration, the characteristics of movement of soil water and salt under different cumulative infiltration were studied. the results indicated that when the salinity of the infiltration water was 3g / l, the top soil was desalinized and salt accumulated at the wetting front

    通過對不同入滲下土壤鹽運移規律的室內模擬試驗研究,結果表明利用礦化度為3g l入滲后,土壤從上至下逐漸脫鹽,上層土壤含鹽於土壤初始含鹽,中間土層基本保土壤初始含鹽值,但濕潤鋒附近發生突變,含鹽大值。
  18. Dry matter and yield decrease with salt increasing on same irrigation level. ( 4 ) the minimal soil moisture content increases with salt content increasing. meeting minimal needs, crop yield is satisfactory in the soil with salt content bellow 0. 6 %, but not in soil salt content above 0. 6 %, so planting in this soil is n ' t suggested

    ( 4 )隨著土壤鹽分增加作物對土壤分要求也增加,含鹽0 . 6 %以下的土壤滿足分要求,可獲較理想產,大於0 . 6 %以保土壤分狀態減輕或消除鹽分脅迫的措施已經不可行,建議不使用含鹽> 0 . 6 %的耕地。
  19. 2 the comparisons between soil water deficiency in natural and artificial forest land show that : ( 1 ) the concept of " forestland steady moisture capacity " is presented and defined as the lowest soil water content that can not affect the forest regular growth primarily and cause inverse succession in community

    2天然林地和人工林地土壤分虧缺狀況對比: ( 1 )提出了「林地土壤穩定」的概念,初步定義為「不會影響到林分正常生長、發育,不會導致群落產生逆向演替所需的土壤含」 。
  20. The nitrogen between minimum protein content and maximum yield were the nitrogen of coordinated variation of yield and grain protein content in 50 % or 60 % of soil water content

    蛋白質含值和產高值之間對應的施氮為產和蛋白質含在土壤分含為田間的50 %和60 %條件下協同變化的施氮區間。
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