3,274 research outputs found

    In-situ cosmogenic <sup>36</sup>Cl denudation rates of carbonates in Guizhou karst area

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    This study quantifies surface denudation of carbonate rocks by the first application of in-situ cosmogenic &lt;sup&gt;36&lt;/sup&gt;Cl in China. Concentrations of natural Cl and in-situ cosmogenic &lt;sup&gt;36&lt;/sup&gt;Cl in bare carbonates from Guizhou karst areas were measured with isotope dilution by accelerator mass spectrometer. The Cl concentration varied from 16 to 206 ppm. The &lt;sup&gt;36&lt;/sup&gt;Cl concentrations were in range of (0.8–2.4)×106 atom g−1, resulting in total denudation rates of 20–50 mm ka−1 that averaged over a 104–105 a timescale. The &lt;sup&gt;36&lt;/sup&gt;Cl-denudation rates showed roughly a negative correlation with the local mean temperature. This preliminary observation may suggest the variations of proportions of chemical weathering and physical erosion in denudation process, depending upon local climatic conditions

    (1-Oxo-2,6,7-trioxa-1-phosphabicyclo­[2.2.2]octan-4-yl)methyl 4-methyl­benzene­sulfonate

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    In the title compound, C12H15O7PS, the P atom has a distorted tetra­hedral environment. The P—O—C—C torsion angles deviate significantly from zero [average = 12.0 (3)°], indicating that the bicyclic OP(OCH2)3C cage is strained. In the crystal, weak C—H⋯O inter­actions consolidate the packing
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