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Kinetics of enzymatic unhairing by protease in leather industry 总被引:2,自引:0,他引:2
In leather industry, unhairing is a heavy pollution operation. The conventional lime-sulfide process produces a large amount of sulfide which is toxic to health and difficult to dispose. Moreover, conventional lime-sulfide process leads to the destruction of the hair causing increased COD, BOD and TDS loads in the effluent. As an alternative method, enzymatic unhairing is a promising clean technology. The main utilized enzyme preparations are proteases.There are many reports about enzymatic unhairing, most of which are qualitative. The kinetics of enzymatic unhairing by protease was discussed in this article. It will provide useful information to enzymatic unhairing. In our research, by analysis of the concentrations of released total protein in enzyme bath during protease unhairing, the good linearity between released total protein and square root of time (min1/2) was obtained at the initial stage. The good linearity suggests that enzymatic unhairing by protease is a diffusion-controlled process at the initial stage. The analysis of kinetics of released saccharides also confirms the same conclusion. On the other hand, the same characteristics between the kinetics of released saccharides and that of released total protein further confirms that it is the hydrolysis of core protein by protease that leads to the degradation of proteoglycans and the release of protein and saccharides. However, in our tests, the kinetics of released collagen indicates that the injury to skin took place in 3-6 h. Therefore, it’s necessary to control the time of protease unhairing within an appropriate limit. 相似文献
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黄土丘陵沟壑区地形和土地利用对深层土壤有机碳的影响 总被引:5,自引:4,他引:1
研究地形和土地利用对深层土壤有机碳(soil organic carbon,SOC)的影响,对准确评估土壤固碳潜力和土壤碳循环具有重要意义.以3种地形(峁顶、峁坡、沟底)和7种土地利用类型(农田、果园、天然草地、人工与天然灌木林、人工与天然乔木林)为对象,在黄土丘陵沟壑区燕沟流域采集53个0~1m土壤剖面中6个层次,898个土壤样品,研究了地形和土地利用方式对黄土丘陵沟壑区小流域深层SOC含量和分布影响.结果表明,地形、土地利用方式、土层深度及其两两交互作用对流域深层SOC空间分布有极显著影响(p0.01).深层(10~100cm)与表层(0~10cm)SOC在3种地形的分布不同.对于表层土壤(0~10cm),峁坡SOC含量(10.7g·kg-1)最高,其次是沟底(8.9g·kg-1),峁顶最低(4.4g·kg-1);对深层土壤有机碳,沟底最高(5.6g·kg-1),峁坡次之(4.5g·kg-1),峁顶最低(3.2g·kg-1).深层SOC空间分布因土地利用方式存在显著差异.与农田相比,果园0~40cm土层SOC含量降低21%,但80~100cm土层SOC含量提高13%;天然灌木林40~100cm平均含量(5.3g·kg-1)较农田高66%(p0.05);但天然乔木林40~100cm与其它土地利用方式差异较小.沟底深层(20~100cm)SOC储量(5.04kg·m-2)最大,占1m剖面SOC储量的71.4%;峁坡占63.6%;峁顶占72.3%.深层(20~100cm)SOC储量天然灌木林最高,为6.01kg·m-2,占1m剖面SOC储量的64.7%,天然乔木林深层相对储量最小,仅占49.7%;农田和果园深层相对储量均达到70%以上. 相似文献
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Preliminary report on methane emissions from the Three Gorges Reservoir in the summer drainage period 总被引:3,自引:0,他引:3
Fei Lu Le Yang Xiaoke Wang Xiaonan Duan Yujing Mu Wenzhi Song Feixiang Zheng Junfeng Niu Lei Tong Hua Zheng Yongjuan Zhou Jiangxiao Qiu Zhiyun Ouyang 《环境科学学报(英文版)》2011,23(12):2029-2033
Considerable variations may exist in CH4 emissions from the Three Gorges Reservoir. 相似文献
298.
A new type of sponge iron sphere (NSIS) with 1-5 mm diameter, made of concentrated iron powder and possessed high activity and intension, was prepared by mini-pellet sintering integrated with H2 direct reduction. Static state experiment has been carried on to investigate the Cd2+ removal efficiency from wastewater by the NSIS and to explore the Cd2+ removal reaction kinetics. It was suggested that initial pH value and Cd2+ original concentration had significant influence on Cd2+ removal percentage. Cd2+ removal percentage decreased significantly with the increasing of Cd2+original concentration whether the original pH value be adjusted to 3.0 or without adjustment. The results showed that the Cd2+ removal process followed the first order reaction because the reaction order was from 0.803 to 0.996. The apparent reaction rate constant between Cd2+ and NSIS was from 0.0025 to 0.1000 (mg·L?1)1-n·min?1. Compared with SIS reduced by charcoal reduction, NSIS deoxided by hydrogen possessed higher activity, and could remove the same quantity of Cd2+ within a shorter period of time. 相似文献
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湛江特呈岛红树林区底泥TOC的释放研究 总被引:1,自引:0,他引:1
以湛江特呈岛红树林区为考察对象,通过底泥TOC向上覆海水释放的模拟对比实验,研究了红树林区底泥中TOC的释放规律和泥水比、温度、pH值三个环境因子对TOC释放的影响,同时对静态和动态体系底泥TOC的释放进行了对比。结果表明,静态下,不同条件释放规律一致,上覆海水TOC的变化呈近似"W"的趋势;泥水比增大会使底泥向上覆海水的TOC释放量增加;温度对底泥TOC释放的影响较为复杂,上覆海水温度较高或较低都有利于底泥TOC的释放;碱性条件有利于沉积物中TOC的释放;海水的运动对沉积物TOC的释放有很好的促进作用。 相似文献