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1.
Due to the ambient temperature fluctuation during the process of storage, transportation, and sale, frozen fillets may go through frozen-thawed cycles that result in quality changes. In order to detect the frozen-thawed cycles in frozen tilapia fillets, near infrared spectroscopy was applied. The thawing loss, cooking loss, moisture content, total volatile basic nitrogen, and texture profile of fillets in seven frozen-thawed cycles were analyzed to reflect the change of quality. A total of 60 fillets were used to collect the spectra on both dorsal and belly flesh in frozen and thawed state from the first to the seventh cycle. The results showed that there is a better discrimination among the once and the repeated frozen-thawed samples in the frozen state than the thawed state. Frozen samples were still conducive to the differentiation and had higher classification accuracy, ranging from 80% to 93.33%. Dorsal flesh was more beneficial for the differentiation than belly flesh and had the highest accuracy, ranging from 86.67% to 93.33% in the frozen state. These results showed that the nondestructive and fast detection of repeated frozen-thawed cycles in frozen tilapia fillets can be accomplished by near infrared spectroscopy, which has enormous potential for practical application.  相似文献   
2.
以黄淮海平原潮土区的砂壤土和黏壤土为研究对象,通过培养试验研究了干湿交替(干湿频率分别为0、2、6、12次)和外源氮(2种土壤中添加氮累计量均为220 mg N·100g~(-1)干土)下砂壤土和黏壤土的CO_2和N_2O释放模式的影响。结果表明,干湿交替和外加氮源显著激发了砂壤土和黏壤土的CO_2和N_2O的释放速率:干燥期越长,外加N源对土壤CO_2释放速率的激发效应越强;干燥期越短,外加N源对土壤N_2O释放速率的激发效应越强。两种土壤的CO_2和N_2O的释放速率对干湿交替的响应模式一致,砂壤土的碳氮矿化速率对干湿交替响应更为强烈,砂壤土的可溶性有机碳和无机氮(NO-3和NH+4)含量及温室气体排放速率均高于黏壤土。在外加氮源的条件下,干湿交替显著提高了砂壤土和黏壤土中可溶性有机碳和无机氮的含量,增大了实际生产中农田土壤无机氮淋失和温室气体排放的可能性。  相似文献   
3.
[目的]对W-OH砒砂岩固结体干湿循环特性及其细观机理进行研究,为实现W-OH固结改良砒砂岩及其耐久性研究提供科学依据。[方法]采用W-OH(亲水性聚氨酯材料)对砒砂岩进行固结处理,基于无侧限抗压试验、三轴抗压试验,研究其在干湿循环条件下的力学性能,并结合SEM,EDS和称重法对其干湿循环后样品微观结构、元素和质量损失进行分析,以获得其破坏机理。[结果]W-OH砒砂岩固结体的无侧限抗压强度、弹性模量和黏聚力在1~3次干湿循环后升高;在3~9次干湿循环后,固结体的力学强度降低;9次之后,剩下高黏结力的W-OH胶结体包裹于砒砂岩颗粒表面,力学强度趋于稳定。内摩擦角在1~9次干湿循环后上下波动,9次干湿循环后趋于稳定。采用碳元素分析和质量损失分析相结合的方法对土样中W-OH流失特性进行评价,发现土样在1~9次干湿循环中W-OH胶结体逐渐降低,并在9次干湿循环后达到稳定,这与上述宏观力学变化的规律相似,验证了破坏机理,为判断其长期特性提供理论依据。[结论]研究表明可将9次干湿循环后达到稳定的W-OH砒砂岩固结体的力学性质作为土体的长期力学特性。  相似文献   
4.
Submerged rice paddies are a major source of methane (CH4) which is the second most important greenhouse gas after carbon dioxide (CO2). Accelerating rice straw decomposition during the off-rice season could help to reduce CH4 emission from rice paddies during the single rice-growth season in cold temperate regions. For understanding how both temperature and moisture can affect the rate of rice straw decomposition during the off-rice season in the cold temperate region of Tohoku district, Japan, a modeling incubation experiment was carried out in the laboratory. Bulk soil and soil mixed with 2% of δ13C-labeled rice straw with a full factorial combination of four temperature levels (?5 to 5, 5, 15, 25°C) and two moisture levels (60% and 100% WFPS) were incubated for 24 weeks. The daily change from ?5 to 5°C was used to model the freezing–thawing cycles occurring during the winter season. The rates of rice straw decomposition were calculated by (i) CO2 production; (ii) change in the soil organic carbon (SOC) content; and (iii) change in the δ13C value of SOC. The results indicated that both temperature and moisture affected the rate of rice straw decomposition during the 24-week aerobic incubation period. Rates of rice straw decomposition increased not only with high temperature, but also with high moisture conditions. The rates of rice straw decomposition were more accurately calculated by CO2 production compared to those calculated by the change in the SOC content, or in its δ13C value. Under high moisture at 100% WFPS condition, the rates of rice straw decomposition were 14.0, 22.2, 33.5 and 46.2% at ?5 to 5, 5, 15 and 25°C temperature treatments, respectively. While under low moisture at 60% WFPS condition, these rates were 12.7, 18.3, 31.2 and 38.4%, respectively. The Q10 of rice straw decomposition was higher between ?5 to 5 and 5°C than that between 5 and 15°C and that between 15 and 25°C. Daily freezing–thawing cycles (from ?5 to 5°C) did not stimulate rice straw decomposition compared with low temperature at 5°C. This study implies that to reduce CH4 emission from rice paddies during the single rice-growth season in the cold temperate regions, enhancing rice straw decomposition during the high temperature period is very important.  相似文献   
5.
麦冬是我国传统中药之一,兼备保健和治疗作用。为了探究麦冬能否应用在宠物食品中,本试验以不同浓度的麦冬水提物(3.91~8000μg/mL)为受试药物,从细胞的形态、增殖、凋亡及周期4个方面对猫肾细胞(F81)进行安全性评价。结果表明:在试验浓度范围内,麦冬水提物没有抑制F81的增殖,且在3.91~62.5μg/mL的浓度范围内,凋亡及周期结果经统计学分析均无显著性差异,与对照组接近,且细胞形态良好。说明在一定浓度范围内,麦冬水提物对F81细胞无毒害作用。  相似文献   
6.
Tang DQ  Wei YQ  Yin XX  Lu Q  Hao HH  Zhai YP  Wang JY  Ren J 《Fitoterapia》2011,82(6):920-926
Quercetin's protective effects on the glomerulosclerosis of diabetic nephropathy (DN) in rat mesangial cells were investigated. The cell cycles, type IV collagen and laminin, TGF-β1 mRNA, Smad 2/3 and Smad 7, and activities of cell antioxidases were measured. Compared with the high glucose group, quercetin may decrease the cell percentages of G0/G1 phase, Smad 2/3 expression, laminin and type IV collagen, and TGF-β1 mRNA level significantly. The antioxidant capacity, the cell percentages of S phase and Smad 7 expression was significantly increased by quercetin. These results suggest that quercetin is a protective agent against glomerulosclerosis in DN.  相似文献   
7.
高性能耐磨纸的研究   总被引:4,自引:0,他引:4  
探索了不同的涂布量、胶粘剂的种类和用量对耐磨纸的耐磨转数、吸水高度和湿强度的影响,通过优化涂布工艺配方使耐磨纸的耐磨转数提高到7000转以上。  相似文献   
8.
土壤冻融交替生态效应研究进展   总被引:20,自引:2,他引:20  
孙辉 《土壤》2008,40(4):505-509
土壤冻融作用是高纬度和高海拔地带性土壤热量动态的一种表现形式.国际上关于冻融的研究多集中在北方高纬度地带,特别是苔原、泰加林和北极生态系统,越来越集中在全球变化对冻融生态系统土壤过程的效应方面.已有研究表明冻融作用会引起土壤团聚结构破坏并导致冻融侵蚀、土壤溶液中养分浓度升高而导致土壤养分流失、土壤解冻后还可能导致土壤呼吸和N素矿化以及一些痕量气体短时间释放增加等,这些研究表明了冻融过程对土壤物理、化学、生物等各方面的效应.我国有大面积北方季节性地带冻土和青藏高原高海拔冻土,而在土壤冻融作用及生态效应方面的工作较少,值得关注和深入研究.  相似文献   
9.
The amounts of N2O released in periods of alternate freezing and thawing depend on site and freezing conditions, and contribute considerably to the annual N2O emissions. However, quantitative information on the N2O emission level of forest soils in freeze‐thaw cycles is scarce, especially with regard to the direct and indirect effect of tree species and the duration of freezing. Our objectives were (i) to quantify the CO2 and N2O emissions of three soils under beech which differed in their texture, C and N contents, and humus types in freeze‐thaw cycles, and (ii) to study the effects of the tree species (beech (Fagus sylvatica L.) and spruce (Picea abies (L.) Karst.)) for silty soils from two adjacent sites and the duration of freezing (three and eleven days) on the emissions. Soils were adjusted to a matric potential of –0.5 kPa, and emissions were measured in 3‐hr intervals for 33 days. CO2 emissions of all soils were similar in the two freeze‐thaw cycles, and followed the temperature course. In contrast, the N2O emissions during thawing differed considerably. Large N2O emissions were found on the loamy soil under beech (Loam‐beech) with a maximum N2O emission of 1200 μg N m–2 h–1 and a cumulative emission of 0.15 g N m–2 in the two thawing periods. However, the sandy soil under beech (Sand‐beech) emitted only 1 mg N2O‐N m–2 in the two thawing periods probably because of a low water‐filled pore space of 44 %. The N2O emissions of the silty soil under beech (Silt‐beech) were small (9 mg N m–2 in the two thawing periods) with a maximum emission of 150 μg N m–2 h–1 while insignificant N2O emissions were found on the silty soil under spruce (0.2 mg N m–2 in the two thawing periods). The cumulative N2O emissions of the short freeze‐thaw cycles were 17 % (Sand‐beech) or 22 % (Loam‐beech, Silt‐beech) less than those of the long freeze‐thaw cycles, but the differences between the emissions of the two periods were not significant (P ≤ 0.05). The results of the study show that the amounts of N2O emitted in freeze‐thaw cycles vary markedly among different forest soils and that the tree species influence the N2O thawing emissions in forests considerably due to direct and indirect impacts on soil physical and chemical properties, soil structure, and properties of the humus layer.  相似文献   
10.
研究鲢(Hypophthalmichthys molitrix)在冷冻-解冻过程中的品质变化规律。鲢于–18℃条件下冻藏10 d,流水解冻后再贮藏于–18℃条件下,5 d后解冻,共反复冷冻-解冻5次。在解冻1、3、5次后随机取3条鲢测定其解冻损失、蒸煮损失、硬度、咀嚼性、恢复性、硫代巴比妥酸(TBA)值、L*值、b*值、盐溶性蛋白(SSP)含量、Ca2+-ATP酶活性、总巯基含量、表面疏水性和感官值等指标,评价反复冷冻-解冻对鲢品质的影响。结果表明,在第1次冷冻-解冻时,硬度、咀嚼性、恢复性、盐溶性蛋白(SSP)含量和Ca2+-ATP酶活性与鲢初始值相比显著降低(P<0.05),b*值和表面疏水性显著升高(P<0.05);解冻损失、L*值和TBA值在第3次冷冻-解冻时显著上升(P<0.05);总巯基含量在第5次冷冻-解冻时显著下降(P<0.05);而蒸煮损失在冷冻-解冻过程中没有显著变化(P>0.05);感官值在第5次冷冻-解冻时为47,感官品质已不可接受。各指标变化表明,鲢品质会随着反复冷冻-解冻次数增加而下降,在运输、贮藏和销售过程中要防止温度波动,避免反复冻融对鲢品质造成不利影响。  相似文献   
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