岩石-土壤-四川牡丹元素迁移体系中的微生物效应

[目的]研究四川牡丹岩土环境背景以及微生物在元素迁移过程中的作用,为了解营养元素的表生地球化学行为规律及微生物在元素迁移体系中的作用提供理论依据。[方法]利用ICP-OES测定四川牡丹生境母岩、土壤以及种子的大量(P,S,K,Ca,Na,Mg,Al)、微量(Fe,Mn,Cu)营养元素含量,同时利用Illumina高通量测序技术测定根际土壤中细菌、真菌的组成和结构。[结果](1)四川牡丹生长土壤以弱碱富钙为主要特征,元素组成基本保留了母岩特征;(2)元素从母岩到土壤中的迁移富集系数排序为:CaNaSPMgKAlFeMnCu,植物吸收系数排序为:PSKCuMgCaNaMnFeAl;(3)碱土金属淋溶率和铝铁率对土壤细菌的多样性(Alpha)影响显著,但对真菌的影响不显著;(4)P,Mn的迁移主要受母岩控制,而Ca,Mg,Fe,S等元素的迁移富集受到了微生物的影响。[结论]细菌和真菌在元素迁移体系中的作用相似,主要参与Fe,S,Mg,Ca的相关反应过程。     

1047年北宋宫廷祈雨的诸相

本文以1047年发生在北宋宫廷内的一场祈雨祭祀为研究对象,运用"剧场国家"理论,描绘了祈雨的"展演"相与"权力"相,研究了祈雨期内以展演为表征、以权力为暗流的人神、人地、人人关系。研究发现:一方面,祈雨是充满象征意义的展演式活动,祈雨人宋仁宗需要向天神与黎民展演德行,而展演德行又需借助于气象技术;另一方面,贾昌朝被罢相是多重因素作用下的结果,罢相反映出北宋中期朝廷内激烈的政治纷争,其仍为庆历新政后权力博弈的延续。可见这场祈雨是一场德行的展演,也是实在的操纵帝国的权力之争。     

Comparative analysis of different methods revealing the involvement of proteins during ageing of rice seeds

Seed longevity is a very important characteristic controlling seed quality. However, the mechanism underlying this characteristic is poorly understood. In this study, 'FH7185', a storable rice variety, the germination rate of which was 66.63%, much higher than the control after artificial ageing under relative humidity 88% and 42°C for 21 days. Different methods were applied to reveal the involvement of proteins during ageing of rice seeds. In total, 35 differential proteins were identified from 2D‐PAGE, and 3,719 proteins from iTRAQ analysis. A comparison of these two methods showed that not all protein types could be detected on the 2D‐PAGE gels, and the dynamic range was somewhat limited. So the comprehensive proteome map from the iTRAQ analysis was used to identify the quantitatively regulated proteins that played roles in seed longevity, and found that the most marked change was the increased abundance of many metabolic enzymes, especially the ones involved in α‐linolenic acid metabolism in the embryos during ageing. OsLOX2 and OsLOX3 had a negative effect on seed longevity, which were lower in FH7185 than the control. The dehydrogenase (LOC_Os07g44430) which played a major catalytic role in lipid peroxidation, also changed significantly during ageing. Therefore, OsLOX2, OsLOX3 and Loc_OS 07G44430 may be involved in the regulation of seed longevity with a synergistic effect.     

新时期科研院所党建工作的几点思考

阐述了新时期科研单位加强党建工作的重要性,提出了新形势下抓好科研单位党建工作的基本原则,即坚持围绕发展、服务中心,坚持与时俱进、改革创新,坚持以人为本、突出主体,坚持突出重点、务求实效。同时,提出了新时期科研院所党建工作创新的着力点,即在工作思路上、在工作定位上、工作内容上,工作机制上、工作方法上等进行创新。     

冲击式速冻设备上下送风速度对虾仁冻结过程的影响

随着人们对速冻食品品质的要求不断提高,商家对食品速冻技术的要求也在不断提高,冲击式速冻技术作为目前先进的速冻技术之一成为研究热点。但由于其高速射流冲击导致的内部换热区流场的不均匀会造成设备换热效率差,能效比低等问题。为找到使得设备换热区流场最优的送风速度,该文以明虾虾仁为研究对象,利用数值模拟结合试验验证的方法研究了冲击式速冻设备中上下送风速度对虾仁冻结过程的影响,分为上下两侧风速保持一致且同时改变;上侧送风速度为15 m/s、下侧为0~15 m/s;以及下侧送风速度为15 m/s、上侧为0~15 m/s 3个试验组进行研究。研究结果为:当冲击式速冻设备两侧送风速度保持一致时,随着风速的增大,虾仁冻结时长缩短但减小幅度也会不断减小;当上下两侧送风速度大小相差悬殊时,两股冲击射流相对冲击会在低速侧形成促进虾仁表面流场流动的涡流,提高换热效率,减小虾仁冻结时长;当上下两侧送风速度大小相差不大时,两股冲击射流相对冲击会在虾仁表面形成流速较低的射流"真空区",降低虾仁换热效率,增大虾仁冻结时长;在试验的两侧送风速度范围内,当上侧送风速度为15 m/s,下侧送风速度为2 m/s时,虾仁对流换热强度最大,冻结时长最短。     

有机质浸染砂水泥土的力学特性及本构关系

为研究海南省海湾地区分布的有机质浸染砂水泥土的力学特性,该文首先对有机质浸染砂水泥土和标准砂水泥土进行无侧限抗压强度对比试验(采用配合比均为熟石灰掺入比7.5%、水泥掺入比20%、水灰比0.45),定量分析养护龄期对其无侧限抗压强度及试样破坏形式的影响。然后对有机质浸染砂水泥土进行单轴抗压试验,获得了水泥土材料的应力-应变全过程曲线、刚度变化规律以及改进邓肯-张本构模型。结果表明:1)有机质浸染砂水泥土试样的破坏类型为塑性剪切破坏和脆性剪切破坏;2)有机质浸染砂水泥土抗压强度随着养护龄期的增加基本呈指数形式增长,但在养护龄期14 d后,增长速度逐渐降低并趋于稳定;3)随着养护龄期增长,水泥土刚度增加。在加载初期,水泥土切线模量随着轴向应变增加而增大,呈现刚度硬化现象;4)基于单轴抗压试验得到应力-应变全过程曲线,可分为2个阶段:塑性阶段、软化阶段;5)通过对应力-应变全曲线的描述,得到了修正的邓肯-张模型,确定模型参数后,与实测数据对比发现,该修正模型可以模拟有机质浸染砂水泥土的应力-应变关系。     

“森林资源诅咒”的存在性、传导机制及破解对策:综述与展望

文中研究森林资源丰裕度与经济增长的关系，从森林资源诅咒的存在性检验、传导机制和破解对策3个方面对国内外相关文献进行了梳理总结。结果表明:森林资源诅咒研究已经取得了一定成果，但是现有文献对森林资源诅咒现象的实证研究结果不稳定，会因研究对象、时间、样本以及模型和指标选取的不同而变化；现有研究对森林资源诅咒的传导机制缺乏实证检验，在指标选择和模型构建中尚存在许多不足之处。未来研究需要考虑指标筛选的科学性、计量模型的稳健性以及中介和调节效应的引入等；此外，森林资源丰裕度与经济增长之间的关系可能不是线性关系，因此在建立计量模型时应对模型形式进行优化选择。     

Effect of soil acidification on the growth and nitrogen use efficiency of maize in Ultisols

Purpose

To examine the effect of soil acidification on growth and nitrogen (N) uptake by maize in Ultisols.

Materials and methods

A clay Ultisol derived from Quaternary red earth and a sandy Ultisol derived from tertiary red sandstone were used in this study. A pot experiment was conducted with maize growing in the two Ultisols acidified to different pH values. Urea with ¹⁵N abundance of 10.11% was used to investigate the distribution of N fertilizer between soil and plant. Total N content and ¹⁵N abundance in plant and soil samples were determined by elemental analysis-isotope mass spectrometry.

Results and discussion

Critical soil pHs of 4.8 and 5.0 were observed for maize growing in the clay and sandy Ultisols, respectively. Below the critical soil pH, increasing soil pH significantly increased maize height and the yield of maize shoots and roots (both P < 0.05), but changes in soil pH showed no significant effect on maize growth above the critical soil pH in both Ultisols. Maize growing in the sandy Ultisol was more sensitive to changes in soil pH than in the clay Ultisol. Increase in the pH in both Ultisols also increased N accumulation in maize, the N derived from fertilizer in maize, physiological N use efficiency, and N use efficiency (NUE) by maize. Changes in soil pH had a greater effect on these parameters below the critical soil pH, compared to above. The change in soil pH had a greater effect on N accumulation in maize, the N derived from fertilizer in maize, and NUE in the sandy Ultisol than in the clay Ultisol. The NUE increased by 24.4% at pH 6.0, compared with pH 4.0 in the clay Ultisol, while the NUE at pH 5.0 was 4.8 times that at pH 4.0 in the sandy Ultisol. The increase in soil pH increased the ratio of N accumulation in maize/soil residue N and decreased the potential loss of fertilizer N from both Ultisols.

Conclusions

Soil acidification inhibited maize growth, reduced N uptake by maize, and thus, decreased NUE. To maintain soil pH of acidic soils above the critical values for crops is of practical importance for sustainable food production in acidic soils.

     

Remediation of saline-sodic soil using organic and inorganic amendments: physical,chemical, and enzyme activity properties

Purpose

Crops grow poorly in saline-sodic soils, and the productivity of these soils can be dramatically improved with proper amendments. Current research mainly focuses on either organic or inorganic soil amendments, whereas few studies address options of combining organic and inorganic amendments. The objective of this study was to develop new organic and inorganic soil amendments which can lower the soil pH, replace sodium, and improve soil structure.

Materials and methods

Polyhalite (PL), microporous potassium-silicon-calcium mineral fertilizer (MF), furfural residue (FR), and fulvic acid (FA) were mixed with four different ratios to produce organic and inorganic soil amendments: PLFR, PLFA, MFFR, and MFFA. And their optimum mixing ratios were determined by comparing the potassium, calcium concentrations, and pH of filtrate after dissolution. Then, a leaching experiment was conducted by packing mixtures (mass ratio of soil to amendment = 219:1, equivalent to 13 t/hm²) of the saline-sodic soil with each one of these amendments plus two contrasts, gypsum (GP), and no amendment (CK). And the remediation effect was compared by pH, EC, ESP, texture, organic recombination degree of clay, saturated hydraulic conductivity, water-stable aggregates fraction, and enzyme (urease, alkaline phosphatase, and catalase) activities of soil.

Results and discussion

After four times leaching experiment, soil treated with PLFR had lower pH and 25.86% lower exchangeable sodium than untreated soils. The water-stable small macroaggregate fractions and saturated hydraulic conductivity of the MFFR-treated soils were significantly increased by 133% and 31%, respectively. Also, the total soil and heavy fraction organic carbons of the soils treated with MFFR in addition to its alkaline phosphatase activity were all significantly higher than the other treatments.

Conclusions

The results revealed that MFFR has more potential as a soil amendment to improve soil structure and quality and thus help in the development and use of saline-sodic lands for agriculture.

     

我国橡子资源的开发利用

橡子营养丰富，而且具有多种功能特性，广泛应用在食品和其它工业中。对橡子仁、橡子皮质和橡子壳的成分、功能和应用等研究情况进行了综述，并介绍了橡子资源在食品及其它工业领域的应用进展，以及提出了橡子资源开发与研究过程中遇到的问题和解决方案。