Geochemical Mass Balance and Elemental Transport during the Weathering of the Black Shale of Shuijingtuo Formation in Northeast Chongqing, China

Figure 5

Mass transfer coefficient of (a) Si, (b) Al, (c) Na, (d) K, (e) Ca, (f) Mg, and (g) Fe versus strain calculated using Ti.

(a)

(b)

(c)

(d)

(e)

(f)

(g)