賈第蟲（Giardia）間接免疫熒光檢測(cè)試劑盒

廣州健侖生物科技有限公司

廣州健侖長(zhǎng)期供應(yīng)各種生物原料，主要代理品牌：美國(guó)Seracare、西班牙Certest、美國(guó)Fuller、美國(guó)NOVABIOS、 Cellabs等等。

Cellabs公司是一個(gè)的生物技術(shù)公司，總部位于澳大利亞悉尼。專門研發(fā)與生產(chǎn)針對(duì)熱帶傳染性疾病的免疫診斷試劑盒。其產(chǎn)品40多個(gè)國(guó)家和地區(qū)。1998年，Cellabs收購TropBio公司，進(jìn)一步鞏固其在研制熱帶傳染病、寄生蟲診斷試劑方面的位置。

賈第蟲（Giardia）間接免疫熒光檢測(cè)試劑盒
    該公司的Crypto/Giardia Cel IFA是國(guó)標(biāo)*推薦的兩蟲檢測(cè)IFA染色試劑、Crypto Cel Antibody Reagent是UK DWI水質(zhì)安全評(píng)估檢測(cè)的*抗體。

主要產(chǎn)品包括：隱孢子蟲診斷試劑，賈第蟲診斷試劑，瘧疾診斷試劑，衣原體檢測(cè)試劑，絲蟲診斷試劑，錐蟲診斷試劑等。

廣州健侖生物科技有限公司與cellabs達(dá)成代理協(xié)議，歡迎廣大用戶咨詢訂購。

我司還提供其它進(jìn)口或國(guó)產(chǎn)試劑盒：登革熱、瘧疾、流感、A鏈球菌、合胞病毒、腮病毒、乙腦、寨卡、黃熱病、基孔肯雅熱、克錐蟲病、違禁品濫用、肺炎球菌、軍團(tuán)菌、化妝品檢測(cè)、食品安全檢測(cè)等試劑盒以及日本生研細(xì)菌分型診斷血清、德國(guó)SiFin診斷血清、丹麥SSI診斷血清等產(chǎn)品。

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【Seracare產(chǎn)品介紹】

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【公司名稱】 廣州健侖生物科技有限公司
【】    楊永漢 
【】 
【騰訊 】 2042552662
【公司地址】 廣州清華科技園創(chuàng)新基地番禺石樓鎮(zhèn)創(chuàng)啟路63號(hào)二期2幢101-3室
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冬季常有溫帶鋒面氣旋來襲，因而盡管全年有雨，秋冬降雨量通常略多于春夏。雨以小雨和小陣雨居多，幾乎沒有雷雨。氣旋頻繁過境，年降雨量500-700mm,在地形有利地區(qū)（如北美洲西北部）多達(dá)2500mm以上。zui冷月平均氣溫在0℃以上，zui暖月又低于22℃，年較差遠(yuǎn)小于同緯度的內(nèi)陸與東岸地區(qū)。屬于這一氣候的有西北歐、加拿大太平洋沿岸、智利南部、澳大利亞東南部、新西蘭等小部分。除亞洲、非洲和南極洲沒有外，其余各大洲都有，其中以歐洲大陸西部及不列顛群島zui為典型。形成這種氣候的主要原因是，本區(qū)位于中緯度(40°～60°)大陸西岸，終年盛吹偏西風(fēng)，風(fēng)從西面海上吹來，沿岸又有暖流，使西風(fēng)更加溫暖濕潤(rùn)，登陸后受地形抬升，即能大量降水。就西歐來說，沿岸的北大西洋暖流很強(qiáng)大，溫度濕度較高，沿岸又特別曲折，地中海、波羅的海等深入內(nèi)陸，再加上西歐的地勢(shì)低平，平原和山地皆呈東西走向，故使西風(fēng)和氣旋等可深入內(nèi)陸，擴(kuò)大了大西洋影響的范圍，使歐洲西部的溫帶海洋性氣候特別典型。1、冬暖夏涼，年溫差小
海洋性氣候區(qū)內(nèi)愈靠近大洋，氣候的海洋性愈強(qiáng)。特別是在冬季，因沿岸有暖流經(jīng)過，西風(fēng)從暖流海面吹來，氣流溫暖潮濕，因此冬季氣溫比同緯度的大陸中心和大陸東岸暖得多。zui冷月均溫均在0℃以上。夏季時(shí)暖流水溫仍較大陸溫度低，海上要比陸上涼得多，這里受西風(fēng)影響zui熱月均溫在22℃以下。由于冬暖夏涼，年溫差要比同緯度其它地區(qū)小得多。
2、全年有雨，冬雨較多
此區(qū)正當(dāng)溫帶氣旋活動(dòng)的路徑上，氣旋雨量豐沛，特別是冬季時(shí)溫帶氣旋更為活躍，雨日很多，但降水強(qiáng)度并不大。冬季降水量在全年所占比例稍大，全年沒有干季，用一句話概括溫帶海洋性氣候的特點(diǎn)：冬無嚴(yán)寒，夏無酷暑。
3、氣溫年變化與日變化都很小
在洋面上甚至觀測(cè)不到日變化。年變化的極值一般比大陸后延1個(gè)月，如zui冷月為2月，zui暖月為8月。在高緯地區(qū)zui冷月還可能是3月，zui暖月也可能到9月。秋季暖于春季。
4、降水量的季節(jié)分配比較均勻
降水日數(shù)多，但強(qiáng)度小。云霧多，濕度高。
In winter, there is often a temperate frontal cyclone, so despite the rain throughout the year, autumn and winter rainfall is usually slightly more than in spring and summer. Most of the rain was light rain and small showers. There was almost no thunderstorm. Cyclones frequently cross the border, with an annual rainfall of 500-700mm, and up to 2500mm above favorable terrain (such as in northwestern North America). The average temperature in the coldest month is above 0°C, and the warmest month is below 22°C. The year-on-year difference is much smaller than that in the inland and east coast regions with the same latitude. The climate that belongs to this area is Northwest Europe, Canada Pacific Coast, South Chile, Southeast Australia, New Zealand and other small parts. With the exception of Asia, Africa and Antarctica, there are other continents, of which the western European continent and the British Isles are the most typical. The main reason for this climate is that the area is located on the west coast of the mid-latitudes (40° to 60°) and it is blowing westwards all year round. The wind blows from the west and the coast has warm currents, making the westerlies warmer and moister. After being lifted by the terrain, it is able to have a lot of precipitation. As far as Western Europe is concerned, the North Atlantic warm coast along the coast is very strong, with high temperature and humidity, and the coastline is particularly twisted. The Mediterranean Sea and the Baltic Sea go deep into the inland. Together with the low-lying plains of Western Europe, the plains and mountains are east-west oriented. The west winds and cyclones can penetrate deep into the interior and expand the range of Atlantic influences, making the temperate marine climate in western Europe particularly typical. 1, cool in winter and cool in summer, with small annual temperature difference
The closer the oceanic climate zone is to the ocean, the stronger the oceanic climate is. In winter, especially in winter, warm winds pass along the coast, and the westerly winds come from the warm currents. The air flow is warm and humid. Therefore, the winter temperatures are much warmer than the continental centers at the same latitude and the east coast of the mainland. The coldest month average temperature is above 0 °C. In the summer, the temperature of the warm current is still lower than that of the mainland, and the sea is much cooler than the land. Here, the average temperature of the hottest month is below 22°C. Because of the cool winter and cool summer, the annual temperature difference is much smaller than other regions at the same latitude.
2, there is rain throughout the year, more winter rain
In this area, the path of extratropical cyclones is rich in cyclone rainfall, especially in winter when the extratropical cyclones are more active and there are many rainy days, but the rainfall intensity is not great. The proportion of winter precipitation in the whole year is slightly larger, there is no dry season in the whole year, and the characteristics of temperate marine climate are summarized in one sentence: winter is not cold, and summer is not very hot.
3. The annual and daily changes in temperature are very small
Even daily changes cannot be observed on the ocean surface. The annual extremes of change are generally one month behind the mainland, such as the coldest month of February and the warmest month of August. The coldest month in high latitudes may also be March, and the warmest month may reach September. Autumn is warm in spring.
4. Seasonal distribution of precipitation is more even
There are many days of precipitation, but the intensity is small. More clouds and more humidity.