木质基材料界面研究进展

介绍了木质基材料的表面和界面，以及木质基材料界面的一些现代研究手段。最后概述了木质基材料界面的研究状况。     

高温预处理玉米秸秆条件的优化

对玉米秸秆高温预处理条件进行优化,以降低还原糖损失率和提高灰分去除率为目的,探讨了高温预处理时料液比、蒸煮温度、蒸煮时间对还原糖得率的影响。通过采用单因素多水平试验方法得到最优预处理条件为料液比1∶7,蒸煮温度118℃,蒸煮时间0.5 h。在此最优条件下,预处理后的秸秆还原糖损失率为1.86%,灰分去除率为35.2%。     

胡椒预处理方式对胡椒脱皮的影响

通过改变胡椒的预处理方式来解决固态发酵脱皮时间短与固态发酵脱皮白胡椒色泽差之间的矛盾。结果表明：不同条件下沸水热烫处理得到的胡椒脱皮率虽能达到100 %,但色泽不理想;而在室温条件下,经不同水处理后脱皮得到的白胡椒的色泽明显比沸水热烫的好,但脱皮率未能达到100 %;用热水浸泡预处理后的实验组不仅胡椒脱皮率能达到100 %,而且色泽也较为理想,已达到市售的水平。所以,选择胡椒脱皮的最优预处理方式为50 ℃热水浸泡20 min。     

基于高光谱技术的茶鲜叶含水率检测与分析

茶鲜叶含水率是茶叶加工业中衡量茶叶品质的一个重要指标。为了实现茶叶加工过程中茶鲜叶含水率的快速检测,本文提出了一种应用高光谱技术分析茶鲜叶含水率的无损检测方法。通过对茶鲜叶高光谱图像感兴趣区域光谱数据的提取,利用4种不同的算法对原始数据进行预处理,采用逐步回归分析法对预处理后的数据提取特征波长,并采用多元线性回归法、偏最小二乘回归建立特征波长和茶鲜叶含水率定量分析模型。研究结果表明,经过卷积平滑处理后的正交信号校正的预处理结合逐步回归分析法所建立的偏最小二乘回归茶鲜叶含水率预测效果最佳,模型校正集、交叉验证集和预测集的相关系数分别为0.8977、0.8342和0.7749,最小均方根误差分别为0.0091、0.0311和0.0371。由此可见,高光谱技术能有效的实现茶鲜叶含水率的检测,这为茶叶加工业中衡量茶叶品质提供了新的检测方法。     

不同NaCl预处理对低温胁迫古巴牛乳树幼苗叶片色素含量的影响

对古巴牛乳树盆栽苗进行不同浓度的NaC1预处理及热激预处理,探索其对低温下古巴牛乳树[Manilkara roxburghiana (Wight) Dubard]叶片色素的影响.结果表明:6‰NaC1预处理能有效缓解古巴牛乳树幼苗叶片受低温伤害,总叶绿素、叶绿素a及叶绿素b均较高于其它处理,此时盆土的实际盐度是3.70‰.     

不同优质粳稻花药对低温和激素处理的培养响应

以3份优质粳稻品种为供试材料,研究了3种低温预处理和9个激素处理组合对离体花药培养的影响。结果表明:供试材料花药对低温预处理的响应存在明显差异,对激素处理组合的响应也存在一定差异。     

香蕉麻预处理脱胶优化研究

天然香蕉麻纤维存在“粗、硬、脆”等问题,影响到常规与高档纺织品的开发;为提高天然香蕉麻可纺性能．在系统分析香蕉麻化学成分的基础上。采用正交试验方法对酶预处理脱胶与双氧水预处理脱胶工艺进行了优化。结果表明,以胶质溶除率评定,酶预处理下最佳脱胶工艺条件是：氢氧化钠浓度8g／L,精炼时间3h,酶处理时间6h;双氧水预处理最佳脱胶工艺条件是：pH9,温度50℃,处理时间30min。     

土壤中铝与各类型表面的吸附及释放机理的研究进展

综述了土壤中铝与各类型表面的吸附反应、铝的吸附对土壤和粘土矿物化学和物理性质的影响、以及土壤中铝的释放过程和机理。     

全子叶生物活性豆腐凝胶特性的研究

通过因子筛选实验,确定了接种量、微生物转谷氨酰胺酶(MTG)用量和水豆比是影响全子叶生物活性豆腐凝胶特性的关键因子。在此基础上,采用响应曲面法(Response SurfaceMethodology,RSM)分别建立了豆腐硬度和持水率的二次多项数学模型,验证了模型的有效性并探讨了上述3个因子的交互作用。从产品成本和凝胶特性综合考虑,选择出最佳配比,即乳酸菌接种量为105cfu/mL,MTG用量为347 U/L,水豆比为8.5,其硬度和持水率实测值分别为44.8g和89.2%,可生产出富含乳酸菌和几乎全部大豆营养的健康豆腐。     

Comparing surface erosion processes in four soils from the Loess Plateau under extreme rainfall events

This research aims to improve erosion control practice in the Loess Plateau, by studying the surface erosion processes, including splash, sheet/interrill and rill erosion in four contrasting soils under high rainfall intensity (120 mm h⁻¹) with three-scale indoor artificial experiments. Four contrasting soils as sandy loam, sandy clay loam, clay loam and loamy clay were collected from different parts of the Loess Plateau. The results showed that sediment load was significantly impacted by soil properties in all three sub-processes. Splash rate (4.0–21.6 g m⁻²∙min⁻¹) was highest in sandy loam from the north part of the Loess Plateau and showed a negative power relation with the mean weight diameter of aggregates after 20 min of rainfall duration. The average sediment load by sheet/interrill erosion (6.94–42.86 g m⁻²∙min⁻¹) was highest in clay loam from middle part of the Loess Plateau, and the stable sediment load after 20 min showed a positive power relation with the silt content in soil. The average sediment load increased dramatically by rill and interrill erosion (21.03–432.16 g m⁻²∙min⁻¹), which was highest in loamy clay from south part of the Loess Plateau. The average sediment load after the occurrence of rill showed a positive power relation with clay content and a negative power relation with soil organic matter content. The impacts of slope gradient on the runoff rate and sediment load also changed with soil properties. The critical factors varied for different processes, which were the aggregate size for splash erosion, the content of silt particles and slope gradient for sheet/interrill erosion, and the content of clay particles, soil organic matter and slope gradient for rill erosion. Based on the results of the experiments, specific erosion control practices were proposed by targeting certain erosion processes in areas with different soil texture and different distribution of slope gradient. The findings from this study should support the improvement of erosion prediction and cropland management in different regions of the Loess Plateau.