木材及木基材料吸湿尺寸稳定性检测方法研究

为实现木材及木基材料吸湿尺寸稳定性横向比较,规范其检测方法,依据现有相关检测标准,借鉴日本工业木材吸湿尺寸稳定性检测方法,结合木质材料特性以及我国的具体情况,提出一种木材及木基材料吸湿尺寸稳定性的检测方法,即以温度20℃、相对湿度65%条件下的材料尺寸为基准,测定在温度40℃、相对湿度为75%和90%的两种吸湿环境条件下的材料尺寸变化。通过该方法对柚木、印茄木、朴木3种不同尺寸的木材和对多层材料、高密度纤维板、普通刨花板3种木基材料的吸湿尺寸稳定性进行测定,以评价该方法的适用性和可行性。结果表明:木材与木基材料试样不超过12 d即可达到吸湿平衡,不同材料尺寸变化率、湿胀系数的大小关系也与实际情况一致。因此木材与木基材料试样均适于用该方法。     

水稻上有机肥部分替代化肥试验小结

通过对有机肥与化肥配合施用田间试验结果分析,我市水稻上有机肥部分替代化肥的适宜比例以有机氮与无机氮比为1：9,这样可有效减少化肥施用,达到化肥减量增效的目的。     

‘王林’苹果苦痘病的防治试验

近几年来‘王林’苹果苦痘病的发病率较高,为了探索防治办法,2018—2019年在瓦房店市驼山乡大魏村‘王林’苹果园进行施用“聚能螯合钙+硅”+生物有机肥试验。结果表明:第1年好果率达到90.2%,比对照提高15.0%;第2年分别为96.82%、22.23%。病果的病斑数也明显减少。     

安徽省作物养分供需分析及化肥减施潜力研究

有机-无机相结合的农田养分管理模式是现阶段中国发展绿色农业的必由之路,因而开展有机、无机养分和作物养分需求的比较研究对促进养分资源的合理分配和施用具有重要的参考价值。本文采用文献调查和统计分析的方法,评估了安徽省16市2010—2016年主要有机肥(包括秸秆、粪便、绿肥和饼肥)的养分资源,明晰了安徽省农业生产中有机、无机养分投入现状,并根据农业种植结构开展了有机、无机养分和作物养分需求的差异和关系研究,最后探索了安徽省的化肥减施潜力。结果表明:安徽省2010—2016年平均有机肥养分资源为287.70万t,N、P_2O_5和K_2O分别为104.49万t、39.60万t和143.61万t,可基本满足作物的养分需求;但有机肥的当季利用率低,N、P_2O_5和K_2O的当季利用率分别为21.44%、19.91%和52.61%,有机肥N、P_2O_5和K_2O实际还田量仅占作物养分需求的20.74%、25.38%和63.61%,占农田养分总投入的比重分别为11.87%、10.27%和51.35%。全省N、P_2O_5、K_2O养分实际投入量(包括有机肥和化肥)是作物养分需求的1.75倍、2.47倍和1.24倍,有7个市的N和13个市的P_2O_5养分施用量超过作物需求的2倍,存在较高的环境污染风险。通过控制农业总养分输入,安徽省的化肥减施潜力为35.12%,N、P_2O和K_2O的减施潜力分别为21.28%、23.97%和78.61%。提高有机肥的当季利用率和发展冬季绿肥资源可进一步促进化肥减施。本研究可为安徽省化肥零增长和农牧业的绿色可持续发展提供数据参考。     

不同处理方法改善桉木渗透性研究

采用3种方法处理尾叶桉,对尾叶桉木材气体渗透性进行了测定,探讨不同处理方法对木材渗透性影响及其作用机理。结果表明:尾叶桉木材因含有侵填体/树胶、导管壁上筛状纹孔影响木材渗透性,木材纵向渗透性大于横向渗透性。经真空、苯-乙醇、尿素处理后,木材渗透性均得到改善;但真空、苯-乙醇处理改善效果不明显,渗透性比未处理材提高幅度均未超过10%;尿素处理可显著改善尾叶桉木材渗透性,渗透性提高了18.91%~41.41%。     

基于PLSR-BP复合模型的红壤有机质含量反演研究

对红壤地区土壤有机质进行快速预测,以满足智慧农业与精准施肥的需要。以江西省奉新县北部为研究区域,采用1 km×1 km标准格网划分研究区进行采样,共得到红壤样本248个。对土壤光谱进行了包含分数阶导数在内的3种数学变换方法,将经过P=0.01显著性检验的波段用于模型的构建,选用偏最小二乘回归(PLSR)和BP神经网络建立土壤有机质含量预测模型。结果表明:当对红壤光谱数据进行1.5阶导数变换后再使用PLSR-BP复合模型对土壤有机质含量进行预测时的结果为最优,训练集R~2=0.89,RMSE=4.68g·kg~(-1),验证集R~2=0.87,RMSE=5.55g·kg~(-1),RPD=2.75。1.5阶导数对红壤光谱数据的变换能够更好地突出与有机质相关的特征信息,有助于其含量预测。PLSR-BP复合模型预测精度优于单一模型,能够较好地预测红壤有机质含量,为精准农业快速监测红壤有机质含量提供了新的途径。     

原料茶干燥工艺对绿茶饮料品质的影响

为探明饮料用原料茶的适宜干燥工艺,将不同干燥方式、干燥程度绿茶原料加工成茶饮料,研究其浸出特性及品质稳定性。结果表明:(1)低温浸提时,茶多酚浸出量以炒干最高,高温时以烘炒焙、烘炒烘处理最高。氨基酸的浸出量则均以烘干、烘焙处理最高。(2)烘干、烘焙样品在灭菌前后及贮藏期间的L值显著为高,平均值较其余处理高2.035~3.905;抗色变能力同样以烘干较强,低温贮藏时的-a/b值较炒干处理样高19.5%。(3)感官风味比较显示,大多数处理茶汤在灭菌后均呈现出绿黄或黄绿色,香气带熟,但烘干处理仍能保持绿明亮,且滋味、香气未显熟味;贮藏期间的风味稳定性也以烘干样为最佳。综合分析,饮料用原料茶的干燥工序宜采用烘干工艺,且烘干程度以5%~6%为佳。     

大豆小肽螯合铁的制备工艺及光谱分析研究

通过铁源筛选比较得知,氯化亚铁比较适合与大豆小肽进行螯合反应制备大豆小肽螯合铁,利用响应面法优化了大豆小肽螯合铁的制备工艺,优化结果为:小肽与亚铁盐质量比4∶1,反应pH5.0,反应温度40℃,得到离子螯合率平均值为56.81%,经中试车间生产试制得到大豆小肽螯合铁的得率是78.3%,螯合率为82.39%,检测大豆小肽螯合铁的主要成分中的蛋白含量为78.94%,铁的含量为10.87%。红外和紫外光谱分析检测结果显示:大豆小肽和大豆小肽螯合铁(Fe~(2+))红外吸收峰的强度在不同波长位置上有明显的变化,大豆小肽螯合铁(Fe~(2+))在紫外波长上发生了明显的位移且宽化,表明大豆小肽螯合铁(Fe~(2+))形成了络合物。同时对大豆小肽螯合铁的结构进行了预测。     

Contrasting development of soil microbial community structure under no-tilled perennial and tilled cropping during early pedogenesis of a Mollisol

A range of agricultural practices influence soil microbial communities, such as tillage and organic C inputs, however such effects are largely unknown at the initial stage of soil formation. Using an eight-year field experiment established on exposed parent material (PM) of a Mollisol, our objectives were to: (1) to determine the effects of field management and soil depth on soil microbial community structure; (2) to elucidate shifts in microbial community structure in relation to PM, compared to an arable Mollisol (MO) without organic amendment; and (3) to identify the controlling factors of such changes in microbial community structure. The treatments included two no-tilled soils supporting perennial crops, and four tilled soils under the same cropping system, with or without chemical fertilization and crop residue amendment. Principal component (PC) analysis of phospholipid fatty acid (PLFA) profiles demonstrated that microbial community structures were affected by tillage and/or organic and inorganic inputs via PC1 and by land use and/or soil depth via PC2. All the field treatments were separated by PM into two groups via PC1, the tilled and the no-tilled soils, with the tilled soils more developed towards MO. The tilled soils were separated with respect to MO via PC1 associated with the differences in mineral fertilization and the quality of organic amendments, with the soils without organic amendment being more similar to MO. The separations via PC1 were principally driven by bacteria and associated with soil pH and soil C, N and P. The separations via PC2 were driven by fungi, actinomycetes and Gram (−) bacteria, and associated with soil bulk density. The separations via both PC1 and PC2 were associated with soil aggregate stability and exchangeable K, indicating the effects of weathering and soil aggregation. The results suggest that in spite of the importance of mineral fertilization and organic amendments, tillage and land-use type play a significant role in determining the nature of the development of associated soil microbial community structures at the initial stages of soil formation.     

Organic farming fosters agroecosystem functioning in Argentinian temperate soils: Evidence from litter decomposition and soil fauna

Benefits of organic farming on soil fauna have been widely observed and this has led to consider organic farming as a potential approach to reduce the environmental impact of conventional agriculture. However, there is still little evidence from field conditions about direct benefits of organic agriculture on soil ecosystem functioning. Hence, the aims of this study were to compare the effect of organic farming versus conventional farming on litter decomposition and to study how this process is affected by soil meso- and macrofauna abundances. Systems studied were: (1) organic farming with conventional tillage (ORG), (2) conventional farming with conventional tillage (CT), (3) conventional farming under no-tillage (NT), and (4) natural grassland as control system (GR). Decomposition was determined under field conditions by measuring weight loss in litterbags. Soil meso- and macrofauna contribution on decomposition was evaluated both by different mesh sizes and by assessing their abundances in the soil. Litter decomposition was always significantly higher after 9 and 12 months in ORG than in CT and NT (from 2 to 5 times in average), regardless decomposer community composition and litter type. Besides, mesofauna, macrofauna and earthworm abundances were significantly higher in ORG than in NT and CT (from 1.6 to 3.8, 1.7 to 2.3 and 16 to 25 times in average, respectively for each group). These results are especially relevant firstly because the positive effect of ORG in a key soil process has been proved under field conditions, being the first direct evidence that organic farming enhances the decomposition process. And secondly because the extensive organic system analyzed here did not include several practices which have been recognized as particularly positive for soil biota (e.g. manure use, low tillage intensity and high crop diversity). So, this research suggests that even when those practices are not applied, the non-use of agrochemicals is enough to produce positive changes in soil fauna and so in decomposition dynamics. Therefore, the adoption of organic system in an extensive way can also be suggested to farmers in order to improve ecosystem functioning and consequently to achieve better soil conditions for crop production.