Science

Both subjects have their own importance in the present era. There are different types of career opportunities available for bioinformatics like:
1. Scientific curator.
2. Gene analyst.
3. Protein analyst.
4. Phylogenetic.
5. Research scientist / associate.
6. Data base programmer.
7. Bioinformatics software developer.
8. Computational biologist.
9. Network administrator / analyst.
10. Structural analyst.
11. Molecular modeler.
12. Bio-statistician.
13. Bio-mechanics.
14. Database programmer.
15. Cheminformatician.
16. Pharmacogenetician.
17. Pharmacogenomics.
18. Research scientist / associate.
I think, you should prefer M.Sc in bioinformatics.
All the best.

Hello Ashutosh,
B.Sc is more of a theoretical approach which deals with various scientific laws, theories and research. If you're interested in research field, you can opt for B.Sc followed by M.Sc. B.Sc is a 3 years course.
On the other hand, B.Tech is an engineering course which deals with how the theoretical concepts can be applied to serve the practical purpose, which involves creating new gadgets and machinery to make various life tasks easier. It is a 4 year course.
Briefing it up, while B.Sc. is a study of scientific discoveries, B.Tech is a study of scientific innovations.
I hope I have been able to answer your queries to your satisfaction. If so, kindly upvote this answer. If you've any further questions, kindly revert.

Soil is a mixture of minerals, organic matter, gasses, liquids, and countless organisms that together support life on earth. Soil is a natural body called the pedosphere which has four important functions: it is a medium for plant growth; it is a means of water storage, supply and purification; it is a modifier of Earth's atmosphere; it is a habitat for organisms; all of which, in turn, modify the soil.
Soil is called the skin of the earth and interfaces with the lithosphere, the hydrosphere, the atmosphere, and the biosphere. The term pedolith, used commonly to refer to the soil, literally translates ground stone. Soil consists of a solid phase of minerals (the soil matrix) and organic matter, as well as a porous phase that holds gases (the soil atmosphere) and water (the soil solution). Accordingly, soils are often treated as a three-state system of solids, liquids, and gases.
Soil is a product of the influence of climate, relief (elevation, orientation, and slope of terrain), organisms, and its parent materials (original minerals) interacting over time. Soil continually undergoes development by way of numerous physical, chemical and biological processes, which include weathering with associated erosion. Given its complexity and strong internal connectedness soil has been considered as an ecosystem by soil ecologists.
Most soils have a dry bulk density (density of soil taking into account voids when dry) between 1.1 and 1.6 g/cm3, while the soil particle density is much higher, in the range of 2.6 to 2.7 g/cm3. Little of the soil of planet earth is older than the pleistocene and none is older than the cenozoic, although fossilized soils are preserved from as far back as the Archean.