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1.
柑橘幼果发育期碳水化合物代谢及其与生长发育的关系 总被引:1,自引:0,他引:1
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。 相似文献
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姜片虫虫体抗原氨基酸的测定 总被引:1,自引:0,他引:1
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。 相似文献
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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. 相似文献
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本试验旨在研究大米草(Spartina anglica Hubb.)中耐盐乳酸菌的分离鉴定及对大米草青贮品质的影响,以期为大米草青贮利用提供技术支持和理论依据。试验采用传统培养法筛选出耐盐浓度为10%的乳酸菌菌株,通过生理生化及16S rDNA序列分析法综合鉴定筛选的菌株,并将其添加到大米草原料中进行青贮效果观察。结果表明:分离获得的42株乳酸菌菌株,耐盐溶度最高为10%的4株乳酸菌均为同型发酵的植物乳杆菌(Lactobacillus plantarum),命名为C1、C2、C3和C4。4株乳酸菌均能提高大米草的青贮发酵品质,其中C4显著提高青贮料的可溶性碳水化合物和粗脂肪含量(P<0.05),显著降低青贮料的氨态氮含量(P<0.05);另外,C4处理组的干物质含量和乳酸含量显著高于其他3个菌株处理组(P<0.05),中性洗涤纤维、酸性洗涤纤维、半纤维素和丁酸含量显著(P<0.05)低于其他3个菌株处理组,青贮效果最佳。 相似文献
7.
Ammonia oxidation, the first step of nitrification, is mediated by both ammonia-oxidizing archaea (AOA) and bacteria (AOB); however, the relative contributions of AOA and AOB to soil nitrification are not well understood. In this study we used 1-octyne to discriminate between AOA- and AOB-supported nitrification determined both in soil-water slurries and in unsaturated whole soil at field moisture. Soils were collected from stands of red alder (Alnus rubra Bong.) and Douglas-fir (Pseudotsuga menziesii Mirb. Franco) at three sites (Cascade Head, the H.J. Andrews, and McDonald Forest) on acidic soils (pH 3.9–5.7) in Oregon, USA. The abundances of AOA and AOB were measured using quantitative PCR by targeting the amoA gene, which encodes subunit A of ammonia monooxygenase. Total and AOA-specific (octyne-resistant) nitrification activities in soil slurries were significantly higher at Cascade Head (the most acidic soils, pH < 5) than at either the H.J. Andrews or McDonald Forest, and greater in red alder compared with Douglas-fir soils. The fraction of octyne-resistant nitrification varied among sites (21–74%) and was highest at Cascade Head than at the other two locations. Net nitrification rates of whole soil without NH4+ amendment ranged from 0.4 to 3.3 mg N kg−1 soil d−1. Overall, net nitrification rates of whole soil were stimulated 2- to 8-fold by addition of 140 mg NH4+-N kg−1 soil; this was significant for red alder at Cascade Head and the H.J. Andrews. Red alder at Cascade Head was unique in that the majority of NH4+-stimulated nitrifying activity was octyne-resistant (73%). At all other sites, NH4+-stimulated nitrification was octyne-sensitive (68–90%). The octyne-sensitive activity—presumably AOB—was affected more by soil pH whereas the octyne-resistant (AOA) activity was more strongly related to N availability. 相似文献
8.
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。 相似文献
9.
石榴果实的糖酸组成及风味特点 总被引:2,自引:0,他引:2
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。 相似文献
10.
Fungal N2O production results from a respiratory denitrification that reduces NO3−/NO2− in response to the oxidation of an electron donor, often organic C. Despite similar heterotrophic nature, fungal denitrifiers may differ from bacterial ones in exploiting diverse resources. We hypothesized that complex C compounds and substances could favor the growth of fungi over bacteria, and thereby leading to fungal dominance for soil N2O emissions. Effects of substrate quality on fungal and bacterial N2O production were, therefore, examined in a 44-d incubation after soils were amended with four different substrates, i.e., glucose, cellulose, winter pea, and switchgrass at 2 mg C g−1 soil. During periodic measurements of soil N2O fluxes at 80% soil water-filled pore space and with the supply of KNO3, substrate treatments were further subjected to four antibiotic treatments, i.e., no antibiotics or soil addition of streptomycin, cycloheximide or both so that fungal and bacterial N2O production could be separated. Up to d 8 when antibiotic inhibition on substrate-induced microbial activity and/or growth was still detectable, bacterial N2O production was generally greater in glucose- than in cellulose-amended soils and also in winter pea- than in switchgrass-amended soils. In contrast, fungal N2O production was more enhanced in soils amended with cellulose than with glucose. Therefore, fungal-to-bacterial contribution ratios were greater in complex than in simple C substrates. These ratios were positively correlated with fungal-to-bacterial activity ratios, i.e., CO2 production ratios, suggesting that substrate-associated fungal or bacterial preferential activity and/or growth might be the cause. Considering substrate depletion over time and thereby becoming limited for microbial N2O production, measurements of soil N2O fluxes were also carried out with additional supply of glucose, irrespective of different substrate treatments. This measurement condition might lead to potentially high rates of fungal and bacterial N2O production. As expected, bacterial N2O production was greater with added glucose than with added cellulose on d 4 and d 8. However, this pattern was broken on d 28, with bacterial N2O production lower with added glucose than with added cellulose. In contrast, plant residue impacts on soil N2O fluxes were consistent over 44-d, with greater bacterial contribution, lower fungal contribution, and thus lower fungal-to-bacterial contribution ratios in winter pea- than in switchgrass-amended soils. Real-time PCR analysis also demonstrated that the ratios of 16S rDNA to ITS and the copy numbers of bacterial denitrifying genes were greater in winter pea- than in switchgrass-amended soils. Despite some inconsistency found on the impacts of cellulose versus glucose on fungal and bacterial leading roles for N2O production, the results generally supported the working hypothesis that complex substrates promoted fungal dominance for soil N2O emissions. 相似文献