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11.
以欧亚种葡萄美人指(Vitisviniferacv.ManicureFinger)为试材,正常光湿为对照,采用正常光偏高湿、偏弱光正常湿度、偏弱光高湿、偏弱光临界高湿、临界弱光偏高湿和临界弱光临界高湿6种处理。试验表明:单一偏弱光处理,葡萄叶片叶绿素含量上升,其余处理叶绿素含量下降;6种处理叶绿体类囊体膜磷酸酯酶活性都低于对照,叶绿体类囊体膜磷酸酯酶活性与光照和湿度有关;正常光偏高湿和偏弱光正常湿度部分芽能分化花原基,但在偏弱光高湿或偏弱光临界高湿花芽分化质量严重下降,临界弱光偏高湿和临界弱光临界高湿几乎未发现花原基;单一的弱光因子比单一的高湿因子对叶绿体类囊体膜磷酸酯酶活性和花芽形态分化影响更大,但弱光与高湿同时存在比单一弱光或高湿因子作用于葡萄时,叶绿体类囊体膜磷酸酯酶活性下降更为显著,花芽更难以形成。  相似文献   
12.
不同副梢处理对赤霞珠葡萄生长和结果的影响   总被引:7,自引:1,他引:7  
试验以3~5年生赤霞珠葡萄(CabernetSauvignon)为试材,对其进行了不同的副梢处理:只留顶端1个副梢、副梢绝后处理、花序以上反复摘心、副梢全留。2年的结果表明:副梢全留(所有副梢全留2~3片叶反复摘心)处理的叶面积指数高,果实的产量和品质高。因此,相对多留副梢叶片,改善了叶幕叶龄结构,提高了果实品质,有利于枝梢成熟。  相似文献   
13.
宗绪岩  王世富  李丽 《蚕业科学》2005,31(4):494-496
对不同pH及阳离子浓度下柞蚕蛹蛋白的溶解性进行了研究。结果表明,柞蚕蛹蛋白的等电点pI为4.2~4.5。测定不同的阳离子对其溶解度的影响顺序为Zn2+>Ca2+>Mg2+>Na+,随着阳离子浓度的增加,蛹蛋白的溶解性增加,当离子浓度超过1.0 mol/L时,其溶解性则降低。  相似文献   
14.
采用标准地调查方法,对初植密度为2 m×2m的银中杨人工林的抚育采伐开始期和采伐强度进行调查研究,确定抚育采伐开始期为8年生时,采伐强度为50%。研究确定了银中杨人工林的经营密度表,以期为生产经营提供依据。  相似文献   
15.
刘蕙兰  张建中 《安徽农业科学》2011,39(36):22457-22460
针对宁夏地区农民传统住宅抗震性差,建筑外围护结构保温性能差,采暖系统能源消耗量大,环境污染严重等问题,提出采用轻钢结构配以轻质保温板材的轻钢结构抗震节能体系,以期为宁夏农村住宅设计提供指导性建议。  相似文献   
16.
光胁迫对沙冬青叶绿素荧光特征和光呼吸的影响   总被引:1,自引:0,他引:1  
使用LI-6400测定乌兰布和沙漠东北缘的沙冬青在不同光合有效辐射下的叶绿素荧光特征和光呼吸变化,进而研究其光破坏防御特征的变化。结果表明,PSⅡ最大光化学量子产量(Fv/Fm)可作为衡量沙冬青光胁迫程度大小指标,有效光化学量子产量(Fv′/Fm′)、总光合速率(Pt)、非光化学猝灭(qN)、光呼吸速率(Rp)和Rp/Pt等指标的光进程曲线临界点值和临界点光强度与Fv/Fm的关系都具有明显的规律性。随着Fv/Fm降低,光胁迫程度增加,导致沙冬青光胁迫的最小光合有效辐射降低。可见,沙冬青光破坏防御的一种策略是在胁迫程度较小时通过提高热耗散和光呼吸相对比值(Rp/Pt)来消耗过剩能量,而在胁迫程度较大时可通过增加抑制热耗散和光呼吸的光合有效辐射实现对过剩光能的消耗。  相似文献   
17.
本试验以1株饲用益生菌解淀粉芽孢杆菌B7(Bacillus amyloliquefaciens B7,B.amyloliquefaciens B7)为研究对象,为了增强其在液态条件下的发酵水平,提高其芽孢发酵工艺优化效率,拟采用测定芽孢吡啶二羧酸(dipicolonic acid,DPA)浓度的方法来代替传统的平板芽孢计数法,以探讨此测定方法在芽孢发酵优化工艺中的可行性。首先,通过单因素试验筛选出对菌株产孢有显著促进作用的因子,进一步通过正交优化试验确定蛋白胨、玉米粉、大米蛋白粉和Mn2+组合的最优水平。结果表明,发酵液中的芽孢浓度与测定的DPA荧光强度呈线性相关,在蛋白胨20 g/L、玉米粉10 g/L、大米蛋白粉20 g/L、Mn2+1.0 mmol/L时发酵48 h,检测到DPA荧光强度达到最大,其相应的芽孢浓度达到7.0×109 CFU/mL。与实验室常用的LB培养基相比,芽孢浓度提高了3.3倍;与工业生产用培养基相比,芽孢浓度提高了2.2倍。本研究为芽孢杆菌发酵过程中芽孢浓度测定提供了一种快速方法,为工业菌株B.amyloliquefaciens B7的发酵提供了一种成分简单且高产芽孢的培养基。  相似文献   
18.
In this study, the changes in vitamin C, l-ascorbic acid (AA) and l-dehydroascorbic acid (DHA) levels in broccoli flower buds were examined during pre-storage and storage periods, simulating refrigerated transport with wholesale distribution and retail, respectively. Broccoli heads were pre-stored for 4 or 7 days at 0 °C or 4 °C in the dark and then stored for 3 days at 10 °C or 18 °C. During storage the broccoli heads were exposed for 12 h per day to three different levels of visible light (13, 19 or 25 μmol m−2 s−1) or a combination of visible light (19 μmol m−2 s−1) and UV-B irradiation (20 kJ m−2 d−1), or they were stored in the dark. The vitamin C content in broccoli flower buds during storage was significantly affected by pre-storage period and temperature. Higher vitamin C levels in flower buds after storage were observed for broccoli heads pre-stored for 4 days or at 0 °C as compared to those pre-stored for 7 days or at 4 °C. Storage temperature also affected vitamin C in broccoli flower buds, with higher levels observed for broccoli stored at 10 °C than at 18 °C. Hence, vitamin C in broccoli flower buds was demonstrated to decrease together with increasing pre-storage period, pre-storage temperature and storage temperature. AA in broccoli flower buds was influenced mainly by storage temperature and to a minor extent by pre-storage temperature. The DHA level and DHA/AA ratio were stable in flower buds of broccoli pre-stored for 7 days, whereas increasing tendencies for both DHA level and ratio were observed after pre-storage for 4 days. These results indicate a shift in the ascorbate metabolism in broccoli flower buds during storage at low temperatures, with its higher rate observed for broccoli pre-stored for shorter time. There were no effects of the light and UV-B irradiation treatments on vitamin C, AA and DHA levels in broccoli flower buds.  相似文献   
19.
We evaluated the re-establishment of an Italian ryegrass pasture by self-seeding on a no-till integrated crop-livestock systems (ICLS) in the southern region of Brazil. This work is part of a long-term experimental protocol initiated in 2003. We tested the effects of various management practices, such as summer crop systems (soybean vs. maize–soybean rotation), stocking methods (continuous vs. rotational) and grazing intensities (low vs. moderate), on Italian ryegrass pasture establishment. In addition, we tested resilience of the system by testing pasture's ability to re-establish following a year without seed head production. The experiment consisted in the rotation, on the same area, of Italian ryegrass pasture grazed by sheep during the winter and up to the end of the grass production cycle, and soybean or soybean-maize grain crops rotation cultivated during the summer. The pasture established itself by self-seeding since 2005. Data were collected in 2011 and 2012 stocking season. The soybean summer crop, continuous stocking and low grazing intensity, all positively affected the production of reproductive tillers in 2011. Grazing intensity in 2011 strongly influenced early vegetative tiller densities (before crop harvest) in 2012. However, none of the grazing intensity or the stocking method treatments affected herbage mass at the end of pasture establishment in 2011 or 2012. On the other hand, the soybean summer crop positively affected pasture establishment, both in term of tiller densities and herbage mass at the end of pasture establishment. The removal of all seed heads in 2011 (preventing seed production) resulted in the total failure of pasture establishment in 2012. Overall, Italian ryegrass establishment by self-seeding relies on the annual replacement of the soil seed bank. This experiment demonstrated that under various stocking methods, moderate grazing intensity and maize or soybean summer crop, Italian ryegrass pasture establishment by self-seeding remains successful even when the stocking periods extended up to the end of the grass production cycle. Self-seeding with moderate grazing intensity ensures successful pasture establishment, reduces labour and costs and allows to increase the stocking period and so animal live weight gain over the grazing season.  相似文献   
20.
Aeolian-fluvial interplay erosion regions are subject to intense soil erosion and are of particular concern in loess areas of northwestern China.Understanding the composition,distribution,and transport processes of eroded sediments in these regions is of considerable scientific significance for controlling soil erosion.In this study,based on laboratory rainfall simulation experiments,we analyzed rainfall-induced erosion processes on sand-covered loess slopes(SS)with different sand cover patterns(including length and thickness)and uncovered loess slopes(LS)to investigate the influences of sand cover on erosion processes of loess slopes in case regions of aeolian-fluvial erosion.The grain-size curves of eroded sediments were fitted using the Weibull function.Compositions of eroded sediments under different sand cover patterns and rainfall intensities were analyzed to explore sediment transport modes of SS.The influences of sand cover amount and pattern on erosion processes of loess slopes were also discussed.The results show that sand cover on loess slopes influences the proportion of loess erosion and that the compositions of eroded sediments vary between SS and LS.Sand cover on loess slopes transforms silt erosion into sand erosion by reducing splash erosion and changing the rainfall-induced erosion processes.The percentage of eroded sand from SS in the early stage of runoff and sediment generation is always higher than that in the late stage.Sand cover on loess slopes aggravates loess erosion,not only by adding sand as additional eroded sediments but also by increasing the amount of eroded loess,compared with the loess slopes without sand cover.The influence of sand cover pattern on runoff yield and the amount of eroded sediments is larger than that of sand cover amount.Furthermore,given the same sand cover pattern,a thicker sand cover could increase sand erosion while a thinner sand cover could aggravate loess erosion.This difference explains the existence of intense erosion on slopes that are thinly covered with sand in regions where aeolian erosion and fluvial erosion interact.  相似文献   
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