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71.
聚环氧琥珀酸钠阻碳酸钙垢性能研究 总被引:11,自引:0,他引:11
研究了聚环氧琥珀酸钠在不同因素下的阻碳酸钙性能。实验结果表明 ,聚环氧琥珀酸钠具有较高的阻垢性能和较好的热稳定性 ,在高钙离子浓度、高温水系统中长时间停留对碳酸钙仍有较强的抑制作用。 相似文献
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本文对国内外下古生界海相碳酸盐岩研究的四个主要方面作了总结:(1)有机质丰度及其影响因素;(2)有机质赋存形式;(3)下古生界海相碳酸盐岩有机质丰度和生烃潜力恢复方法和原理;(4)下古生界海相碳酸盐岩热成熟度研究。这四个方面是评价我国下古生界海相碳酸盐岩勘探前景至关重要的因素,也是近年来我们研究下古生界海相碳酸盐岩的热点和难点问题。 相似文献
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Calcium carbonate (CaCO3) application is widely used to ameliorate soil acidification. To counteract soil and bacterial community response to CaCO3 application in an acidic paddy soil in southern China, a field experiment was conducted with four different dosages of CaCO3 addition, 0, 2.25, 4.5 and 7.5?tons/ha, respectively. After one seasonal growth of rice, soil physicochemical properties, soil respiration and bacterial communities were investigated. Results showed that soil pH increased accordingly with increasing dose of CaCO3 addition, and 7.5?tons/ha addition increased soil pH to neutral condition. Moderate dose of CaCO3 application (4.5?tons/ha) significantly increased soil dissolved organic carbon (DOC) and dissolved organic nitrogen (DON) content, enhanced soil respiration, while the excessive CaCO3 application (7.5?tons/ha) decreased these soil properties. High-throughput sequencing results illustrated that moderate dose of CaCO3 application increased the richness and alpha diversity of soil bacterial community. Compared with control, the relative abundance of Anaerolineaceae family belonging to Chloroflexi phylum increased by 38.7%, 35.4% and 24.5% under 2.25, 4.5 and 7.5?tons/ha treatments, respectively. Redundancy analysis (RDA) showed that soil pH was the most important factor shaping soil bacterial community. The results of this study suggest that proper dose of CaCO3 additions to acid paddy soil in southern China could have positive effects on soil properties and bacterial community. 相似文献
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Oxygenated fuel represents an attractive alternative as an additive for reducing soot emissions.Dimethyl carbonate(DMC) is an oxygenated compound which is a good option to reduce soot,but the detailed characteristics of soot produced from combustion of hydrocarbon fuels blended with DMC are still lacking. The present research studied the nanostructure and reactivity of soot particles in ethylene/DMC normal and inverse diffusion flames. High resolution transmission electron microscopy(HRTEM), X-ray diffraction(XRD), and thermogravimetric analysis(TGA)were used to analyze the nanostructure and reactivity of soot. It was found that DMC addition was effective in decreasing the average weights of soot formed in flames. The results of HRTEM images showed that soot particles obtained with DMC addition showed liquid-like material and tight bonding, and exhibited more highly disorganized layers, which give it higher reactivity than soot obtained without DMC addition. Furthermore, HRTEM was used to analyze soot fringe characteristics consisting of fringe tortuosity, fringe length, and fringe separation. XRD was used to crosscheck the results for fringe separation, and was consistent with HRTEM results. In addition, the mass loss curve of TGA experiments showed that DMC addition could enhance the reactivity of soot particles. 相似文献
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基于稳定碳同位素技术的干旱区绿洲土壤有机碳向无机碳的转移 总被引:2,自引:0,他引:2
应用稳定碳同位素技术测定土壤无机碳稳定碳同位素组成(soil inorganic carbonδ13C,SICδ13C),并对干旱区绿洲土壤无机碳进行区分,结合土壤有机碳(soil organic carbon,SOC)与SIC含量关系进一步探讨SOC向SIC转移的碳量.结果表明,4种类型土壤SICδ13C值差异性极显著(P0.01),风沙土SICδ13C值最高且为正,均值为(0.32±0.04)‰,随土层深度增加而增加,说明风沙土原生性碳酸盐占绝对优势;灌漠土、棕漠土和盐碱土SIC的δ13C均值分别(-0.30±0.24)‰、(-1.96±0.66)‰和(-1.24±0.49)‰,随土层变化均呈先降低后逐渐增大的趋势,说明灌漠土原生性碳酸盐占优势,棕漠土和盐碱土发生性碳酸盐相对前者占优势.风沙土、灌漠土、棕漠土和盐碱土的发生性碳酸盐占SIC比例均值分别为1.33%、4.72%、15.01%、35.71%,均小于50%,说明干旱区绿洲土壤发生性碳酸盐比例总体水平较低.风沙土、灌漠土、棕漠土和盐碱土在土壤发生性碳酸盐形成或重结晶过程中固定土壤CO2的量分别为0.30、2.44、4.96、12.40 g·kg~(-1),其中固定来自大气CO2量平均为0.18、0.79、1.45、8.67 g·kg~(-1),来自SOC氧化分解转化为CO2的量分别为0.06、0.83、1.62、1.86g·kg~(-1),说明盐碱土、棕漠土SOC的贡献相对较高,灌漠土、风沙土较低;对土壤固定CO2量的来源比较发现,风沙土、盐碱土固定土壤CO2的量来自大气CO2量较高,SOC的贡献较低,而灌漠土、棕漠土固定来自SOC氧化分解CO2的量较高,大气贡献较低.研究区整体SOC向SIC的碳转移量介于0.03~2.38 g·kg~(-1)之间,平均每千克土壤固定1.09 g的CO2,说明干旱区绿洲土壤发生性碳酸盐所占比例较低,SOC的贡献较少. 相似文献
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