柑橘幼果发育期碳水化合物代谢及其与生长发育的关系

温州蜜柑幼果在盛花后逐渐生长 盛花后6 d开始大量脱落 日本甜夏橙幼果在盛花后12 d内重量未增加，一直处于急剧落果期。甜夏橙幼果中蔗糖含量高出温州蜜柑20多倍，种间还原糖含量变化趋势略有不同。两种柑橘的淀粉含量变化也不同，但它们的淀粉含量与淀粉酶活性、幼果相对脱落率均呈负相关。对幼果碳水化合物代谢与生长、脱落的关系作了讨论。     

蛋白质着色动力学研究

经过蛋白质着色动力学的研究，发现蛋白质着色的行为遵循数学模型Ｙ＝ａＸ＾ｂ。在ｐＨ２－６范围内，蛋白质上染料随染溶ｐＨ的下降而上升，在１５－３０℃温度范围内，蛋白质上染率随温度上升略有提高，当温度超过３０℃时，蛋白质上染率逐渐下降。染浴中添加稀土对蛋白质有较强的促染效果，其实质是染浴中蛋白质首先对稀土高价阳离子进行结合，再通过高价阳离子对色素进吸附。     

Effectiveness of four methods for tagging juveniles of farm-reared gilthead sea bream, Sparus aurata, L.

This study tested different tags for each size of farm-reared gilthead sea bream, Sparus aurata L. juveniles, used in enhancement programmes. The following tags were tested: dye mark, fingerling tag, opercular tag, anchor tag A (filament diameter of 1.20 mm) and anchor tag B (0.85 mm). Tag/mark retention, wounds produced by the tag, ease of application, ease of detection and cost were examined. Epidermal dye marks had poor retention and detection rates. Of the tags tested, retention was greater for the anchor tag A (80–100%) after 7 months; anchor tag B showed a retention rate of only 20% after 3 months. The fingerling tag had a retention rate of 27.5% after 12 months. The opercular tag had a retention rate of 44% after 20 days but fractured the opercular bone in many cases. Tag incisions and wounds persisted in some fish for the duration of the experiment.     

姜片虫虫体抗原氨基酸的测定

本文报道4种方法制备姜片虫虫体抗原,进行氨基酸组成的测定。其氨基酸总量(mg/100ml)结果显示:Ag-F1:608.50;Ag-F2:645.80;Ag-F3:357.14;Ag-F4:501.40;以 Ag-F3总量为最低,但值得重视的是 Ag-F3的丙氨酸(8.34),组氨酸(8.60),甘氨酸(11.00);苏氨酸(12.00),均显著降低。而 Ag-F4的组氨酸(4.80)为17种氨基酸含量最低者。其原因有待探讨。     

套袋对红富士苹果色素及糖、酸含量的影响

 以苹果(Malus pumila) ‘长富2’品种为试材, 研究了套袋对果皮色素及果肉糖、酸含量的影响。结果表明, 套袋果果皮色素、可溶性糖、可滴定酸具有同对照果基本相同的消长规律, 但含量均始终低于对照; 摘袋后果实可溶性糖含量迅速升高, 且花青苷积累速度明显快于对照; 套袋主要降低了果实中山梨醇和蔗糖的含量, 果糖和葡萄糖降低幅度相对较小。     

More evidence that anaerobic oxidation of methane is prevalent in soils: Is it time to upgrade our biogeochemical models?

Estimating future fluxes of CH₄ between land and atmosphere requires well-conceived process-based biogeochemical models. Current models do not represent the anaerobic oxidation of methane (AOM) in land surface soils, in spite of increasing evidence that this process is widespread. Our objective was to determine whether AOM, or potential AOM, commonly occurs in 20 hydromorphic soils spanning a wide range of chemical properties. Bulk soil samples were collected under shallow water near the shoreline of 15 recently drained fish ponds in southern Bohemia (Czech Republic), as well as from below the water table at 3 peatland locations in northeast Scotland and 2 acid sulfate soils on the southern coast of Finland. Each soil slurry was incubated under both oxic and anoxic conditions, with or without the addition of alternative electron acceptors (SO₄²⁻ and NO₃⁻) or H₂PO₄⁻. Here, “oxic” and “anoxic” conditions refer to anoxic soil respectively incubated in a headspace containing air or argon. Using the isotope dilution method, we determined the gross production and oxidation rates of CH₄ after 2 days incubation under oxic headspace conditions, and after 2, 21 and 60 days incubation under anoxic conditions. Large differences in net CH₄ fluxes were observed between soil types and between incubation conditions. AOM was detected in each of the 20 bulk soil samples, which spanned >6 pH units and 2 orders of magnitude in organic C content. Significant positive relationships were found between AOM and gross CH₄ production rates under anoxic conditions, resulting in AOM rates that were sometimes higher than CH₄ oxidation rates under oxic headspace conditions. There was no relationship between net and gross CH₄ production rates, such that 2 soil types could display similar low net rates, yet conceal very large differences in gross rates. The effects of alternative electron acceptors on AOM were idiosyncratic and resulted in no net trend. We did find, however, a negative effect of SO₄²⁻ and H₂PO₄⁻ on gross CH₄ production rates under anoxic and oxic conditions respectively. Under oxic headspace conditions, CH₄ oxidation was related to soil organic C content. Taken collectively, our results suggest that AOM, or potential AOM, is prevalent over a wide range of soil types, that AOM may contribute substantially to CH₄ oxidation in soils, and that AOM in soils should be integrated to current process-based CH₄ cycling models.     

碳纳米管的酸化处理对碳纳米管/聚氨酯复合材料微观结构及性能的影响

对多壁碳纳米管进行酸化处理,并采用原位聚合法制备了碳纳米管/聚氨酯复合材料。利用X射线光电子能谱分析(XPS)、电子扫描显微镜(SEM)、动态力学分析(DMA)研究了碳纳米管酸化与否对复合材料性能的影响。结果表明,碳纳米管经酸化处理后产生了羧基,碳纳米管的原位加入使得复合材料的储存模量和玻璃化转变温度都有所提高,而且经过酸化的碳纳米管对聚氨酯材料的改性要比未酸化碳纳米管对聚氨酯材料的改性效果更为显著。     

菌株Bacillus sp.CLb芽孢漆酶对染料、模拟染料废水脱色的研究

[目的]研究芽孢杆菌菌株CLb的芽孢漆酶在介体的互作下对不同类型的染料及模拟染料废水的脱色效果。[方法]制备芽孢粗酶液,在介体的互作下,测定具有漆酶活性的粗酶液对活性亮蓝、活性黑、靛红和结晶紫的脱色效果,筛选出对染料脱色有促进作用的漆酶介体,并且研究芽孢漆酶在不同pH条件下对染料和模拟染料废水脱色的影响。[结果]菌株CLb的芽孢漆酶在无介体参与下只能使活性亮蓝和结晶紫脱色。在介体乙酰丁香酮（ACE）的作用下,芽孢漆酶对4种染料的脱色率均超过70%。在pH 7.0条件下,芽孢漆酶浓度为44.74 U/L和介体ACE浓度为1 mmol/L时对模拟染料废水的脱色效果最好,6 h脱色率超过80%。在介体乙酰丁香酮存在,pH 7.0的条件下,菌株CLb的芽孢漆酶对合成染料脱色效率高于pH 9.0时的脱色率。[结论]在介体乙酰丁香酮的存在下,芽孢漆酶对染料和模拟染料废水均具有较好的脱色效果。     

石榴果实的糖酸组成及风味特点

采用高效液相色谱法测定4种石榴成熟期果实中糖和酸的组成,并对其味感值和糖酸组分与果实风味指标间的相关性进行分析。结果表明,石榴果实中可溶性糖组分有蔗糖、葡萄糖、果糖和山梨醇,其中葡萄糖和果糖含量最高,分别占总糖含量的43.84%~48.36%和49.18%~50.67%。4个品种中,"玉石籽"的总糖含量最高,"白皮"的最低。石榴果实中主要有机酸是奎宁酸、琥珀酸、草酸、L-苹果酸、莽草酸、柠檬酸和D-苹果酸,其中"玛瑙籽"的总酸含量最高,"青皮"的最低。石榴果实中果糖的味感值最大、其次是葡萄糖;味感值最大的酸是奎宁酸,其次为柠檬酸。相关性分析结果表明,石榴果实的糖酸比与甜味/酸味比值之间呈极显著正相关,各品种间糖酸比(甜味/酸味比值)的差异主要取决于有机酸的含量,与糖含量无关。综合其风味特点,"青皮"和"玉石籽"是甜味较浓的品种,"白皮"和"玛瑙籽"则是酸味较浓的品种。     

有机改良剂对温室土壤及番茄质量的影响

研究了优培-海藻生物有机肥(Y)、微生物菌肥(W)和腐植酸有机肥对日光温室土壤的理化性质、有效态微量元素含量、酶活性以及番茄品质等方面的影响,旨在探索快速、简易且廉价的土壤改良方法,为日光温室土壤改良及有机蔬菜生产提供理论依据。结果表明,不同土壤改良剂对土壤p H无显著影响,在番茄生育期内土壤p H值始终在7.0以上,没有出现酸化问题;拉秧后,除中量腐植酸有机肥(FM)外,其他各处理均能有效降低土壤EC值并达到极显著水平;各处理对提升有效态Mn、Zn和Fe含量的效果不显著,其中,仅高量腐植酸有机肥处理(FH)能同时提高开花结果盛期0~20 cm和20~40 cm土层的有效态Zn含量,与CK相比,分别增加10.8%和13.2%;不同土壤改良剂均可提高土壤脲酶和蔗糖酶活性;不同土壤改良剂对碱性磷酸酶的酶活性影响较小;微生物菌肥对酸性磷酸酶和过氧化氢酶的酶活性影响相对明显;不同土壤改良剂均能提高番茄可溶性固形物、可溶性糖、可滴定酸和维生素C的含量,其中,中量腐植酸有机肥处理提高了番茄的糖酸比。土壤改良剂可有效改善日光温室土壤特性及番茄品质。