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A Kruskall Wallis multiple comparison test demonstrates that Sq, Sdr and Spc on the surface with the drawing are significantly lower (P < 0.01) than those measured on the remainder of the analysed surfaces of L13.
Therefore, it can be presumed that the analysed surfaces might display a little higher surface charge density, as estimated in the analysis presented in Fig. 6.
Superimpositions revealing shape alteration of the analysed surfaces are presented in Fig. 1.
For all of the analysed surfaces containing the pentapeptides, Si-GLMR Pbf G-CF, Si-GLMR Pbf G-CFPEG-GLMR(Pbf)G-CF and Si-GLMR Pbf G-CF characteristic "immonium ions" H2N+ = HC-R, where R is the side chain group of the Si-PEG-GLMR Pbf G-CF related to glycine, arginine, leucine and methionine were viSi-PEG-GLMR Pbf G-CFectra in the low m/ z range aSi-PEG-GLMR Pbf G-CFpeptideSi-PEG-GLMR Pbf G-CF
Only a few investigations have analysed surfaces formed in other media or have analysed fractured surfaces which relate to the bulk morphology.
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In both methods the analysed surface was identified from field controlled geological maps.
With the use of microelectrochemical cells, the specimen surface area in contact with the electrolyte is limited by the use of glass microcapillaries and the local impedance was defined from the ratio of the local potential to the local current restricted to the analysed surface area.
The TH of the analysed surface water of the study area varies between 86 and 716 mg L−1 (avg. 217 mg L−1) indicating moderately hard to very hard type of surface water.
The physico-chemical parameters of the analysed surface water samples of the Pratapgarh district including statistical measures such as minimum, maximum, average values and standard deviation are given in Table 2.
The calcium hardness of the sampled surface water varied from 30.74 to 100.26 mg/L, with a mean of 55.15 mg/L, while magnesium hardness ranged between 21.02 and 68.31 mg/L, with a mean of 37.16 mg/L All the analysed surface water samples were below the WHO permissible limit of 200 mg/L for magnesium hardness.
The (Na+ + K+)/Cl− molar ratios in the analysed surface water from the Birim River basin were greater than 1 (> 1) (Fig. 5c), indicating that halite, as well as silicate weathering, such as potash plagioclase and sodium plagioclase, was the source Na+ and K+ ions (Lin et al. 2016a).
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