海水鹽度 的英文怎麼說
中文拼音 [hǎishuǐyándù]
海水鹽度
英文
salinity of sea water-
The mineralization temperature is in a range of 90 ~ 300, and the mineralization fluid is a combination of slightly acidic - slightly alkalic precipitations, seawater and magmatic water
其成礦溫度在90 ~ 300之間,成礦流體為低鹽度的弱酸性弱堿性大氣降水、海水和巖漿水的混合溶液。Standard test method for alkalinity in brackish water, seawater, and brines
微鹹水海水和鹽水中堿度的標準試驗方法By simulating river plume evolution under the combined action of tide and estival wind field averaged over many years, we have found that the modeled salinity distribution is consistent with the observed one rather well, which means the river plume development plays an important role in adjusting the salinity distribution in the surface layer of bohai sea
通過檢驗河流羽流在潮汐和渤海夏季多年平均風場共同作用下的發展特徵,發現計算得到的表層海水鹽度分佈與實測值相當吻合,因此可以認為河流羽流發展對于渤海夏季鹽度分佈起著重要作用。The salinity of the earth ' s oceans is about thirty - five parts per thousand, meaning that there are about thirty - five grammes of dissolved solids and gases in one kilogramme of water
地球海洋里的鹽度大約為35 % ,意思是說,在每公斤的水中約含有35克溶解的固體和氣體。Study of the relationship between cell size, chlorophyll content of aegiceras corniculatum mesophyll and seawater salinity by fcm
用流式細胞儀探討桐花樹葉肉細胞大小和葉綠素含量與海水鹽度的關系Based on the two ctd data sets from the cruise of the summertime in 2000 and wintertime in 2001 in bohai sea and the collected historic observed thermohaline data, we analyse systemically the distributional characteristics of temperature, salinity and density in wintertime and summertime in the bohai sea and the results reveal that the current hydrologic characteristics of the bohai sea have some obvious variances relative to the previous research results. in summer there are three low - temperature centers in the middle - layer and underlayer of the middle parts of the bohai strait, liaodong bay - mouth and bohai bay - mouth, but there is a uniform high - temperature center in the middle part of the bohai sea. in winter the isotherms extend westward and northward to the bohai sea from the warm core of the bohai strait and a cold - water tongue off the qinhuangdao spreads southeastward out, so the saddle - like isotherm pattern is formed in the middle part of the bohai sea
利用2000年夏季和2001年冬季渤海兩次ctd資料和以前收集的渤海溫鹽調查資料,分析了渤海冬、夏季溫鹽密度的分佈特徵,結果表明,渤海現有的水文特徵與以往研究結果相比發生了明顯的變異:夏季在渤海海峽、遼東灣口和渤海灣口中部中、下層存在三個低溫中心,在渤海中部則出現一個上下均勻一致的高溫中心;冬季等溫線以渤海海峽暖中心向西和向北兩個方向伸入渤海,而從秦皇島外海有一冷水舌向東南方向伸展,在渤海中部海域形成「馬鞍狀」等溫線結構。The results showed the mass abrasion resistance of the wpc was not affected by the immersion time and the saltness of the artificial simulated seawater obviously
研究結果表明:海水的浸泡時間和海水鹽度對塑木復合材料的質量磨損量均無明顯影響。Shipment traffic usually is heavy in littoral area, the navigation capability is required in many riverway. navigation lock was set to suit for the water level ' s variety caused by tide. for a long period, being lack of the quantified assessment on the influence of saltwater intrusion, approaches that freshwater is inpoured to the lock chamber are adopted lest the high concentration salt water be imported to the inland waterway, when the navigation lock is in operation. but such manner should not be reasonale enough
沿海地區船運發達,很多河道有通航要求,為克服潮汐造成的水位變化而設置船閘。長期以來,由於缺乏對鹽水入侵內河河道產生影響的定量評估,在船閘運行過程中為防止高鹽度鹹水入侵內河,通常採用將內河淡水打入閘室的方式來調節通航水位,船閘的這種運行方式不盡合理。A survey of 1000 australians ' perceptions of recycled and desalinated water shows that authorities face a tough time overcoming the public ' s distaste for drinking or bathing in recycled water
一項研究就1000名澳大利亞人對回收水及去鹽海水的看法進行了調查,結果顯示,政府要消除公眾對飲用回收水或用回收水沐浴的厭惡將度過一段艱難歲月。For environmental concerns, a proper design of the brine outfall is essential to enable the end discharge mix rapidly with the ambient coastal waters
出於環境保護考慮,保證海水淡化后產生的高鹽度尾液能夠迅速與受納海水摻混的排放口設計顯得尤為重要。Similarly, in coastal regions where rivers dilute the sea, salinity is somewhat lower than in other oceanic areas
同理,在江河稀釋海水的海岸地帶,海水鹽度略低於其它海區。Salinity temperature depth recorder
海水鹽度溫度深度記錄器The effects of sea water temperature and salinity on the growth and survival of tegillarca granosa larvae and juveniles
海水溫度和鹽度對泥蚶幼蟲和稚貝生長及存活的影響The typical monsoon in this area has a great influence on the oceanic productivity and the salinity of the sea water
本區特有的季風氣候對大洋生產力和海水鹽度的變化都有較大的影響。Special emphasis was put on the plant ' s suitability with its submerged life in seawater, especially its adaptation to the salinity of seawater
其中著重討論了大葉藻與海洋沉水生活相適應的一些特點,特別是其對海水鹽度的適應機理。Glenn noted the water that percolates out from normally irrigated soil, technically known as irrigation return flow, is often as salty as 10 percent seawater
格倫指出,從淡水灌溉的土壤滲出的水,專業名稱叫做「迴流」 ,通常它的含鹽度也相當于像海水鹽度的10 % 。It is used for quality control in research and clinical laboratories. it can be used to check and maintain stock solutions and dilutions
手持鹽度儀是為測量氯化鈉鹽溶液含鹽食品及海水鹽水的濃度而設計的。But on the later condition the trend of accumulation turned to be stable in the w3 treatment ( vseawater / v pure water = 1 ) - in root zone soil, variation of sar value accorded with total salt accumulations and sometimes decreased at the treatment where the v seawater / v pure water > 1. contents of cl - and na + which were the main ions and leached obviously in 0 - 60cm soil were greatly influenced by rainfall, but the rainfall did not affected the contents of ca2 +, mg2 + and k + whose ability of leaching is worse than that of cl - and na + in the root zone soil obviously. the vertical distribution of salt ions in the 0 - 60cm soil were mainly affected by the ratio of v seawater / v pure water in the irrigation water on the condition of not enough rainfall, but on the cont
海水灌溉下,耕層土壤中鹽分含量受降雨量影響很大,足夠的降雨條件下,鹽分不會積累,降雨量較低時,鹽分積累明顯,但在50海水處理下趨于平衡狀態;耕層土壤sar值的變化情況和鹽分含量變化情況相一致,在灌溉水中海水濃度大於50時有所下降;土壤中主要鹽離子為cl ~ -和na ~ + , 0 - 60cm土層內, na ~ + 、 cl ~ -明顯的向土壤底層遷移,其在土壤中的含量受降雨影響顯著,而ca ~ ( 2 + ) 、 mg ~ ( 2 + )和k ~ +在土壤中遷移能力較低,其含量受降雨影響較小; 0 - 60cm層次土壤鹽分的縱向分佈在降雨量較低的條件下主要受灌溉水中海水濃度的影響,而在降雨充分的條件下,地面覆蓋程度成為重要的影響鹽分和水分脅迫下菊芋的生理響應及其海水灌溉研究因子之一。Hitherto, rescue vehicles have relied on acoustic communications links which are susceptible to [ 3 ] varying temperature and saline conditions in the water column
至到今天,目前服役的救生艇仍舊沿用受海水溫度和鹽份變化影響較大的音響通信裝置。Besides the aridity climate, the reason caused the high salinity of the lake water possibly was the frequent transgression in the early and middle permian
造成湖泊水鹽度較高的原因,除了乾旱的氣候外,認為主要是由於早、中二疊世三塘湖地區頻繁的海侵作用造成的。分享友人