一款老人助力起身智能马桶研究

研究一款能在现有旧式马桶基础上,通过加装助力起身智能马桶盖,实现助力起身和智能冲洗的结合,简化操作动作,适应老人使用的设备。     

民国老茶罐里识茶香——记泉祥茶庄的那些事

本文以民国时期较为盛行的茶叶包装为切入点,以"泉祥"老字号茶庄的马口铁茶叶罐为研究对象,通过解读茶叶罐上的图案等蕴含的历史文化信息,梳理了"泉祥"茶庄沉浮起落的发展历程,折射了中国茶文化及工商文化的发展变迁。     

古泰山女儿茶考述

泰山女儿茶,是中国古代北方茶区的特色。笔者在对泰山女儿茶的古籍文献进行梳理的基础上,探究了泰山女儿茶的植物种类,并为"《红楼梦》中提到的女儿茶是泰山女儿茶"这一观点提供了论据。     

校院两级管理模式下地方农业高校教科研指标体系构建探索与对策研究

校院两级管理是高等院校内部管理体制改革创新的必然趋势,对高等院校盘活存量、激活增量具有重要作用。文章系统梳理了国内外高等院校内部管理体制改革和校院两级管理模式以及教科研指标体系的差异和特征,着重聚焦当前地方农业高校教科研指标体系构建中存在的问题,探析地方农业高校校院两级管理教科研指标体系构建的关键因素和环节,提出了“核心+特色”校院两级指标设置和“个人+团队”教师考核评价方式的两项对策,以期为地方农业高校校院两级管理教科研指标考核和评价提供借鉴和参考。     

岩溶流域典型农业区水体氢氧同位素的空间异质性及形成机制

分别于平水期和枯水期采集了花溪河流域典型农业区地表水和地下水样品。利用氢氧同位素示踪技术,结合土地利用类型对研究区不同水体的补给来源、季节变化及主要影响过程进行了分析,并对不同水体氢氧同位素值进行了空间插值分析,同时对其形成机制进行了分析,阐明了不同土地利用类型影响下的主要水文过程。结果表明:(1)研究区不同水体的主要补给来源为当地大气降水,月亮湖水库受蒸发作用影响明显,地表水和地下水的δD和δ~(18)O整体上呈现平水期高于枯水期的特征。(2)地下水的δD和δ~(18)O在枯水期与平水期均呈现明显的空间分异性特征,西部水田/水库集中区富集,东部旱地集中区贫化,土地利用对研究区环境水文过程影响明显。该研究结果有助于了解不同土地利用方式下地表水对地下水的影响,为流域管理提供科学依据。     

不同比例缓释肥、烟草专用复合肥配施对植烟土壤肥力及烤烟产质量的影响

为探究不同比例缓释肥、烟草专用复合肥配施对植烟土壤肥力及烤烟产质量的影响,在宣威市热水镇植烟区设置了5种不同肥料配比组合和对照,对植烟土壤及烤后烟叶进行取样分析。结果表明：不同比例缓释肥配施烟草专用复合肥使土壤综合肥力指数(IFI)相较于CK（单施烟草专用复合肥）提高了12.50%~23.21%,以60%~100%缓释肥等比替代复合肥(T3、T4、T5)表现最优。从烤烟综合品质来看,不同比例缓释肥替代烟草专用复合肥使烤烟综合品质平均得分相较于CK提高了0.19%~6.64%,其中以80%缓释肥替代复合肥处理(T4)表现最优。烤后烟叶经济效益也以T4最优,公顷产值达到59995.80元,高于对照和其他处理。综上所述,缓释肥和复合肥比例为80%:20%,能较好的提高烟叶综合品质,烤后烟叶能获得较好的经济效益,并在一定程度上改善土壤养分结构。     

基于高通量测序及分离培养初步研究美国大豆中真菌多样性

中国是全球最大的大豆进口国,进境大豆所携带的病原真菌传入我国的风险极高。基于高通量测序技术对6批美国大豆真菌多样性进行分析,同时采用分离培养获得单一菌株,依据菌落形态、显微结构及分子技术进行鉴定。高通量测序结果显示,大豆中所有真菌共计5门15纲35目63科112属155种,主要为链格孢属(Alternaria)、球腔菌科(Mycosphaerellaceae)、小戴卫霉科(Davidiellaceae)、小囊菌科(Plectosphaerellaceae)、赤霉属(Gibberella)、附球霉属(Epicoccum)、间座壳属(Diaporthe)、隐球菌属(Cryptococcus)。分离培养结果显示,得到真菌共计40株10种,分别是大豆北方茎溃疡病菌(Diaporthe phaseolorum var.caulivora)、大豆南方茎溃疡病菌(Diaporthe phaseolorum var.meridionalis)、大豆拟茎点种腐病菌(Diaporthe longicolla/Phomopsis longicolla)、大豆炭腐病菌(Macrophomina phaseolina)、尖孢镰刀菌(Fusarium oxysporum)、菌核菌(Sclerotinia sclerotiorum)、镰刀菌(Fusarium sp.)、附球菌(Epicoccum sp.)、交链孢菌(Alternaria sp.)、小双胞腔菌(Didymella sp.)。     

贺兰山野生大型真菌孢子多样性分析

为探讨贺兰山野生大型真菌孢子的多样性,2012-2016年在内蒙古贺兰山南寺和哈拉乌沟两地进行取样,每个样地分别由5人从沟谷入口处进行拉网式调查,共获得4 000余份样品,经过微观形态观察和基因ITS序列比对,鉴定出8目25科69属189种大型真菌,主要对其孢子形态特征、表面特征及长宽比进行分析,得到如下结论:质量性状上,孢子形态特征和表面特征相互独立;数量性状上,大小孢子长宽比、孢子极端比和平均比均具有一致性和关联性,显示孢子数量特征的稳定性;菌种间孢子质量性状和数量性状具有很强的多样性;按照孢子多样性低、中、高分类,贺兰山野生大型真菌物种数分别为152种、26种和11种;孢子多样性分类为大型真菌鉴别、分类提供了基本依据。     

Assessing the effects of vegetation and precipitation on soil erosion in the Three-River Headwaters Region of the Qinghai-Tibet Plateau,China

Soil erosion in the Three-River Headwaters Region (TRHR) of the Qinghai-Tibet Plateau in China has a significant impact on local economic development and ecological environment. Vegetation and precipitation are considered to be the main factors for the variation in soil erosion. However, it is a big challenge to analyze the impacts of precipitation and vegetation respectively as well as their combined effects on soil erosion from the pixel scale. To assess the influences of vegetation and precipitation on the variation of soil erosion from 2005 to 2015, we employed the Revised Universal Soil Loss Equation (RUSLE) model to evaluate soil erosion in the TRHR, and then developed a method using the Logarithmic Mean Divisia Index model (LMDI) which can exponentially decompose the influencing factors, to calculate the contribution values of the vegetation cover factor (C factor) and the rainfall erosivity factor (R factor) to the variation of soil erosion from the pixel scale. In general, soil erosion in the TRHR was alleviated from 2005 to 2015, of which about 54.95% of the area where soil erosion decreased was caused by the combined effects of the C factor and the R factor, and 41.31% was caused by the change in the R factor. There were relatively few areas with increased soil erosion modulus, of which 64.10% of the area where soil erosion increased was caused by the change in the C factor, and 23.88% was caused by the combined effects of the C factor and the R factor. Therefore, the combined effects of the C factor and the R factor were regarded as the main driving force for the decrease of soil erosion, while the C factor was the dominant factor for the increase of soil erosion. The area with decreased soil erosion caused by the C factor (12.10×10³ km²) was larger than the area with increased soil erosion caused by the C factor (8.30×10³ km²), which indicated that vegetation had a positive effect on soil erosion. This study generally put forward a new method for quantitative assessment of the impacts of the influencing factors on soil erosion, and also provided a scientific basis for the regional control of soil erosion.