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91.
三丁基锡对牡蛎超氧化物歧化酶的影响 总被引:6,自引:1,他引:6
本文从牡蛎中提纯超氧化物歧化酶(SOD),分析了氯化三丁基锡(TBTC1)对体外牡蛎SOD部分性质的影响,结果表明:随着TBTC1含量的增加及作用时间的延长,SOD的活力逐渐降低。当TBTC1(Sn含量为600μg/cm^3)作用SOD 24h时酶活力保留50%,到36h时酶活力完全丧失;TBTC1能使牡蛎SOD的耐热、耐酸碱能力降低;PAGE显示,随着TBTC1含量的增加,SOD同工酶谱带逐渐消失;Cu^2 能使失活的SOD恢复部分酶活性。 相似文献
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In this paper, we examined the role of bedrock groundwater discharge and recharge on the water balance and runoff characteristics in forested headwater catchments. Using rigorous observations of catchment precipitation, discharge and streamwater chemistry, we quantified net bedrock flow rates and contributions to streamwater runoff and the water balance in three forested catchments (second‐order to third‐order catchments) underlain by uniform bedrock in Japan. We found that annual rainfall in 2010 was 3130 mm. In the same period, annual discharge in the three catchments varied from 1800 to 3900 mm/year. Annual net bedrock flow rates estimated by the chloride mass balance method at each catchment ranged from ?1600 to 700 mm/year. The net bedrock flow rates were substantially different in the second‐order and third‐order catchments. During baseflow, discharge from the three catchments was significantly different; conversely, peak flows during large storm events and direct runoff ratios were not significantly different. These results suggest that differences in baseflow discharge rates, which are affected by bedrock flow and intercatchment groundwater transfer, result in the differences in water balance among the catchments. This study also suggests that in these second‐order to third‐order catchments, the drainage area during baseflow varies because of differences between the bedrock drainage area and surface drainage area, but that the effective drainage area during storm flow approaches the surface drainage area. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献
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利用精密量热仪测定了MgCl_2、MgCl_2·2H_2O、MgCl_2·4H_2O和MgCl_2·6H_2O在298.15°K溶于水的积分溶解热,并利用Pitzer电解质溶液的。~ΦL方程,计算了溶质的相对表观摩尔热焓,从而得到标准溶解焓分别为(KJ·mol~(-1))—155.86±0.17、—79.45±O.17,—41.78±O.18和—14.58±0.16;晶格能分别为—2490.36,—3158.37,—3772.70和—4376.56。二、四、六水合物的标准生成焓分别为—1289.39,—1898.72和—2497.58;水合焓分别为—76.41,—114.08和—141.28。 相似文献
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S. H.?Withers R. E.?PealeEmail author A. F.?Schulte G.?Braunstein K. M.?Beck W. P.?Hess R. J.?Reeder 《Physics and Chemistry of Minerals》2003,30(7):440-448
Calcite crystals were grown from solution with single-crystal dimensions up to 3 mm and doped up to 0.1 at% with Nd3+ ions. Phase purity was verified by powder X-ray diffraction. The concentration of Nd3+ was measured by energy-dispersive spectrometry and Rutherford backscattering spectrometry. Micro X-ray fluorescence mapping of the calcite grains indicates uniform Nd distribution in as-grown crystal grains. X-ray absorption fine structure suggests that Nd3+ is substituted for Ca2+ with local lattice distortion. Temperature-dependent near-infrared spectroscopy of Nd3+ impurities in calcite reveals large inhomogeneous linewidths and smooth line profiles that are characteristic of glassy hosts, though the samples are well crystallized. 相似文献
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