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Labeled samples are generally difficult to obtain as the labeling step if often performed manually.
The dealloyed samples are generally more reactive at lower overpotentials, but less reactive at higher overpotentials.
SPVs of the extracted samples are generally larger than that of the un-extracted ones.
Pores in the shale samples are generally under 10 µm in size.
In contrast, the Tafel slopes for the dealloyed samples are generally higher, most above 175 mV/dec.
In addition, the concentration of dissolved ions in groundwater samples are generally governed by lithology, nature of geochemical reactions and solubility of interacting rocks (Nosrat and Asghar 2010).
Similar indication were also spotted in the Dearing plot (Dearing et al. 1997), showing that all samples are generally located in the PSD + multiple domain range (Fig. 3c).
FT-IR spectrum of initial and final vermicomposted samples are generally obtained in the mid-infrared area range of 4000 400 cm−1.
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Samples were generally analysed in duplicates.
Less gritty samples were generally regarded as 'more pleasant' by the participants of the study.
The samples were generally counted within 4 24 h after the blood sample was taken.
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