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Quantitative chemical analyses conducted prior to 1947 mainly utilized so-called wet analytical methods, in which the mineral sample is first dissolved.
The sample is first excited with a low-incident power density equal to 70 W·cm−2.
In this scheme, the sample is first analyzed by PGA, which is followed by IPAA and INAA.
The maternal red blood cell (RBC) sample is first incubated with human anti-D antibody, and then indicator Rh(D -positive cells are aD -positive
The video sample is first normalized, and then, the face and its components are detected using the Viola-Jones detection algorithm [68, 69].
This sample is first diluted with 50 μl PBS and then mixed with equal volume of 1% LMA and proceed for the experiment (Bajpayee et al. 2005).
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In this method, the seawater sample was first processed by removing nitrite and ammonium.
The sample was first allocated across 29 provinces, each of which was taken as a universe.
Each sample was first sieved in wet conditions using a 3 − φ sieve.
Each sample was first weighed and then placed into a 5 ml test tube.
The sample was first stratified by geopolitical region.
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