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贾第虫（Giardia）间接免疫荧光检测试剂盒

广州健仑生物科技有限公司

广州健仑长期供应各种生物原料，主要代理品牌：美国Seracare、西班牙Certest、美国Fuller、美国NOVABIOS、 Cellabs等等。

Cellabs公司是一个*的生物技术公司，总部位于澳大利亚悉尼。专门研发与生产针对热带传染性疾病的免疫诊断试剂盒。其产品畅销全球40多个国家和地区。1998年，Cellabs收购TropBio公司，进一步巩固其在研制热带传染病、寄生虫诊断试剂方面的*位置。

贾第虫（Giardia）间接免疫荧光检测试剂盒
    该公司的Crypto/Giardia Cel IFA是国标*推荐的两虫检测IFA染色试剂、Crypto Cel Antibody Reagent是UK DWI水质安全评估检测的*抗体。

主要产品包括：隐孢子虫诊断试剂，贾第虫诊断试剂，疟疾诊断试剂，衣原体检测试剂，丝虫诊断试剂，锥虫诊断试剂等。

广州健仑生物科技有限公司与cellabs达成代理协议，欢迎广大用户咨询订购。

贾第虫（Giardia）间接免疫荧光检测试剂盒我司还提供其它进口或国产试剂盒：登革热、疟疾、流感、A链球菌、合胞病毒、腮病毒、乙脑、寨卡、黄热病、基孔肯雅热、克锥虫病、违禁品滥用、肺炎球菌、军团菌、化妆品检测、食品安全检测等试剂盒以及日本生研细菌分型诊断血清、德国SiFin诊断血清、丹麦SSI诊断血清等产品欢迎致电。

欢迎电话咨询13802525278

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【Seracare产品介绍】

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【公司名称】 广州健仑生物科技有限公司
【联系电话】 13802525278 020-82574011  杨永汉 
【公司传真】 020-32206070
【腾讯 QQ 】 2042552662
【公司地址】 广州清华科技园创新基地番禺石楼镇创启路63号二期2幢101-3室
【企业文化】

冬季常有温带锋面气旋来袭，因而尽管全年有雨，秋冬降雨量通常略多于春夏。雨以小雨和小阵雨居多，几乎没有雷雨。气旋频繁过境，年降雨量500-700mm,在地形有利地区（如北美洲西北部）多达2500mm以上。最冷月平均气温在0℃以上，最暖月又低于22℃，年较差远小于同纬度的内陆与东岸地区。属于这一气候的有西北欧、加拿大太平洋沿岸、智利南部、澳大利亚东南部、新西兰等小部分。除亚洲、非洲和南极洲没有外，其余各大洲都有，其中以欧洲大陆西部及不列颠群岛最为典型。形成这种气候的主要原因是，本区位于中纬度(40°～60°)大陆西岸，终年盛吹偏西风，风从西面海上吹来，沿岸又有暖流，使西风更加温暖湿润，登陆后受地形抬升，即能大量降水。就西欧来说，沿岸的北大西洋暖流很强大，温度湿度较高，沿岸又特别曲折，地中海、波罗的海等深入内陆，再加上西欧的地势低平，平原和山地皆呈东西走向，故使西风和气旋等可深入内陆，扩大了大西洋影响的范围，使欧洲西部的温带海洋性气候特别典型。1、冬暖夏凉，年温差小
海洋性气候区内愈靠近大洋，气候的海洋性愈强。特别是在冬季，因沿岸有暖流经过，西风从暖流海面吹来，气流温暖潮湿，因此冬季气温比同纬度的大陆中心和大陆东岸暖得多。最冷月均温均在0℃以上。夏季时暖流水温仍较大陆温度低，海上要比陆上凉得多，这里受西风影响最热月均温在22℃以下。由于冬暖夏凉，年温差要比同纬度其它地区小得多。
2、全年有雨，冬雨较多
此区正当温带气旋活动的路径上，气旋雨量丰沛，特别是冬季时温带气旋更为活跃，雨日很多，但降水强度并不大。冬季降水量在全年所占比例稍大，全年没有干季，用一句话概括温带海洋性气候的特点：冬无严寒，夏无酷暑。
3、气温年变化与日变化都很小
在洋面上甚至观测不到日变化。年变化的极值一般比大陆后延1个月，如最冷月为2月，最暖月为8月。在高纬地区最冷月还可能是3月，最暖月也可能到9月。秋季暖于春季。
4、降水量的季节分配比较均匀
降水日数多，但强度小。云雾多，湿度高。
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.