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Explain the Bile pigments and salts in urine
The bile pigment, bilirubin (a pigment formed from the destruction of red blood cells), is altered in the intestine to urobilinogen, a coloured substance formed in the intestine from the breakdown of bilirubin. In the urine, the urobilinogen gradually changes to urobilin. In haemolytic jaundice (jaundice due to the breakdown of red blood cells), excretion of urobilin, a brown bile pigment, is increased upto 10 mg daily and in obstructive jaundice (jaundice caused by something blocking the bile duct, for example, gallstones and tumors), it is reduced usually to less than 0.3 mg daily. Bilirubin appears in the urine when there is an appreciable amount of conjugated bilirubin present in the plasma.
Why does marble rarely contain fossils? This is due to of the way that it is formed. When you have a rock that is formed bymetamorphosis then it has been created by heat and pres
Determine in brief about the soil texture The texture is generally determined by the relative proportions of sand, silt and clay. If various size fractions of the particles co
what are the 7 characters of pea plants observed by mendal?
what comes first? egg or chicken?
INTRODUCTION : This exercise is based on here 'Laws and Regulations' of this course. What are we going to do in this exercise? - This might be the question arising in your mind. I
Ask quesdifference between prokaryotic and eukaryotic fatty acid synthesistion #Minimum 100 words accepted#
Define the Nature of Sound This section is a recapitulation of what you have learnt in school. You would recall that sound waves consist of the longitudinal waves of alternate
Experiments with man in space: We have already discussed the usefulness of space flights in Blocks 3&4. One is able to make astronomical observations from satellites; get met
Q.What is soil erosion? The blowing away or washing away of land surface by wind or water is known as soil erosion.
Soil Texture and Methods of Analysis Soil texture is the basic property of a soil related to the size of individual mineral particles, which cannot be easily altered. It spe
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