“…Initial recoveries were three-to fivefold higher for non-exchangeable than exchangeable K, followed by a gradual decline toward a stable level of 240-300 kg ha − 1 , with approximately 3000 kg ha − 1 as the cumulative recovery of non-exchangeable K. The resilient behavior of soil K is further revealed, in that 4 years of crop K removal had no consistent effect on soil concentrations of exchangeable, non-exchangeable or total K, implicating the mineral fraction as an important source of buffering. These findings are to be expected, considering what has long been known about the availability and dynamics of non-exchangeable and mineral K, based on chemical extraction 19,[85][86][87] (see also supplemental references [22] and [27][28][29][30] for the online version of the paper), exhaustive cropping 81,86,88,89 (see supplemental references [8], [15] and [16] for the online version of the paper) and electrodialysis 83,90 .…”