Secondary ferrimagnetic minerals in Welsh soils: a comparison of mineral magnetic detection methods and implications for mineral formation

A range of low-temperature and isothermal magnetic measurements are used to identify the secondary ferrimagnetic mineral (SFM) grain sizes in 10 representative soil samples from Wales. A comparison of percentage frequency-dependent susceptibility (chi(FD) percentage) and low-temperature remanence measurements shows that they are sensitive to different ranges of superparamagnetic (SP) grains, The relative distributions of SP grains and stable single domain (SSD) grains are similar in nine of the samples, Typical distributions for soils dominated by SFMs are approximate to 20-30 per cent SSD and 70-80 per cent SP, Multidomain (MD) grains were not detected in the samples studied. There is evidence that some soils contain significant numbers of ultrafine SP grains < 0.010 mu m that are not detected by low-temperature remanence measurements at 20 K and which will have the effect of depressing values of low-field susceptibility (chi(LF)) and chi(FD) percentage, A :mixing model suggests that chi(FD) percentage may be used semiquantitatively to estimate the proportion of SP grains in a sample. The positively skewed grain-size distributions strongly suggest a mechanism of SFM formation that is driven by processes at the <10(-8) m scale, thus supporting weathering and fermentation as controlling processes, rather than the degradation of SSD bacterial magnetosomes and primary minerals.