The presence of the Brunhes-Matuyama magnetic reversal in deep-sea core sediments makes possible an alternative to the usual K/Ar radioisotope method of dating the reversal as found in rocks. The alternative method uses correlations of Northern
Evaluation of two models to calculate the soil erodibility factor K
The soil erodibility factor K used in the Revised Universal Soil Loss Equation can be calculated by two general applicable models. Data on the various soils covering northern Belgium are processed to evaluate the use of these models. Erodibility
factors are calculated for the top layer of soils where rill and interrill erosion occur. The K-values generated by each model are then compared throughout the range of soil types varying erodibility. For both models average K-values per unit area
Insensible worlds : postrelational ethics, indeterminacy and the (k)nots of relating
Taking up J.-L. Nancy's concept of sense and his ideas around the direction of sense, the A. argues that the insensible is a realm of possibility within the praxis of social and affective norms of sense that may release other modes of being