Figures & data
Table 1. Description of loess samples collected from the Xi Feng loess profile at the CLP
Figure 1. Map of China showing distributions of the CLP as well as major deserts and sand-lands. The loess sampling location is indicated by a black dot.
![Figure 1. Map of China showing distributions of the CLP as well as major deserts and sand-lands. The loess sampling location is indicated by a black dot.](/cms/asset/b767b852-e9f8-476f-9ebc-5476b2a0f49e/uawm_a_10412087_o_f0001g.gif)
Table 2. Massfractions in each layer for TSP, PM 10, PM 2.5, and PM1 size fractions
Figure 2. Relationship between carbonate carbon (CO3 2-C) and water-soluble calcium (Ca2+) for the TSP, PM10, PM2.5, and PM1 fractions of loess.
![Figure 2. Relationship between carbonate carbon (CO3 2-C) and water-soluble calcium (Ca2+) for the TSP, PM10, PM2.5, and PM1 fractions of loess.](/cms/asset/3855ee0f-3396-4e12-a0ec-4c74b9ca54cd/uawm_a_10412087_o_f0002g.gif)
Figure 3. UCC55-normalized abundances for TSP, PM10, PM2.5, and PM1 of loess. Samples for each size fraction represent the average of nine source profiles.
![Figure 3. UCC55-normalized abundances for TSP, PM10, PM2.5, and PM1 of loess. Samples for each size fraction represent the average of nine source profiles.](/cms/asset/c3b06caf-9ab1-4b6a-94de-9b742a9af0db/uawm_a_10412087_o_f0003g.gif)
Table 3. Comparison of elemental ratios (uncertainties) for loess PM and dust-dominated aerosol in source regions
Figure 4. The percentages of crustal and non-crustal origin for elements Pb,Zn, Cr, V, Ni, Cu, and Co of PM2.5 aerosol samples acquired from the ZBT station.15 The fraction of non-crustal origin (f non-crustal origin, in percent) for element X was calculated as follows: f non-crustal origin = 100 × [1 - (Al sample × X loess)/(Al loess × X sample)].
![Figure 4. The percentages of crustal and non-crustal origin for elements Pb,Zn, Cr, V, Ni, Cu, and Co of PM2.5 aerosol samples acquired from the ZBT station.15 The fraction of non-crustal origin (f non-crustal origin, in percent) for element X was calculated as follows: f non-crustal origin = 100 × [1 - (Al sample × X loess)/(Al loess × X sample)].](/cms/asset/4fdd2049-f2ff-468b-a60d-25fcc57fb359/uawm_a_10412087_o_f0004g.gif)