土壤游离氧化铁高光谱特征与定量反演

【目的】建立基于可见-近红外光谱的土壤游离铁精确预测模型,简单、快速、经济地预测土壤游离铁,有助于研究土壤发生和分类。【方法】采集广西壮族自治区的铁铝土、富铁土、淋溶土和雏形土等82个旱地土壤剖面的B层土壤,进行室内土壤化学分析、光谱测定,分析不同光谱变换后的光谱反射率与土壤游离铁含量的相关性。基于特征波段利用偏最小二乘回归(PLSR)和逐步多元线性回归(SMLR)法建立土壤游离铁含量光谱预测模型,通过决定系数(R2)、均方根误差(RMSE)和相对预测偏差(PRD)确定最优模型。【结果】土壤光谱曲线分别在457、800和900 nm波段附近有明显的游离铁吸收和反射峰特征;土壤游离铁含量与原始光谱反射率呈负相关;原始光谱经过微分变换后,游离铁含量与光谱反射率相关性显著提高;基于400～580和760～1 300 nm特征波段和一阶微分光谱变换的SMLR模型预测精度最高,其验证集的R2和RPD分别为0.85和2.62,RMSE为8.41 g·kg~(-1)。【结论】将可见近红外光谱技术应用于土壤游离铁含量高效快速地预测具有良好的可行性。广西旱地土壤光谱反射率与土壤游离铁含量具有高度的相关性,应用逐步多元线性回归方法可以很好地建立土壤游离铁含量反演模型。     

石灰石砂砾负载铁膜及其强化除磷效果

为研究探讨出一种成本低、适用于农村生活污水处理的人工湿地填料负载铁膜方法,通过室内小试比较了石灰石砂砾、普通河沙砂砾2种材料,以及FeCl_3溶液、FeSO_4溶液、Fe(OH)_3胶体溶液3种含铁溶液,并比较了不同的工艺条件,包括4种加液方式:载体浸泡在溶液中不捞出、浸泡2 h后捞出、浸泡1 min后立即捞出和喷淋,3种干燥方式:105℃烘干、太阳晒干和室内自然晾干;同时构建了铁膜石灰石砂砾小型人工湿地,考察了其实际运行效果。试验优选出的负载铁膜方法为:石灰石砂砾浸泡在浓度为1.5 mol·L~(-1)的FeSO_4溶液中,使石灰石砂砾与溶液充分接触1 min后捞出,再将捞出后的石灰石砂砾室内通风自然晾干。铁膜石灰石砂砾对生活污水总磷的静态吸附去除率从普通石灰石砂砾的22.7%提高到80.6%;将其应用于小型人工湿地,总磷去除率比普通石灰石砂砾湿地提高了10%～15%。     

无机碳源对零价铁介导的自养脱氮序批式反应器处理高氨氮废水的影响

无机碳源作为自养微生物的能量来源,是影响自养脱氮细菌富集的重要因素。文章通过添加不同量的KHCO3作为ZVI介导的自养脱氮体系中无机碳源,研究反应体系的脱氮效果影响趋势以及适宜的无机碳源添加量。结果如下:1)KHCO3作为无机碳源可以显著提高NH^+4-N去除率,KHCO3添加量越多,其NH^+4-N去除率越高。KHCO3添加量分别为2 g,1 g,0.5 g的SBR反应器R2,R1,R0.5的NH^+4-N去除率分别为98.39%,65.18%,44.56%,相较不添加KHCO3的R0分别提高86.5%,53.29%,32.67%。ZVI的添加会降低KHCO3对NH^+4-N氧化的促进作用。2)KHCO3可明显提高TIN去除效果,促进总氮脱除的高低顺序是R1>R0.5>R2,SBR反应器R2,R1,R0.5的平均TIN去除率分别为19.01%,32.04%,27.62%,相较于空白组R0分别提高了10.60%,23.63%,19.21%。3)KHCO3可中和硝化反应产生的H^+,对反应体系具有缓冲作用,可使微生物处于较适宜的酸碱环境中,更有利于反应器的稳定运行。4)适量的无机碳源KHCO3可以促进氨氧化细菌和厌氧氨氧化细菌的活性。该研究探讨了无机碳源在零价铁脱氮体系中的影响趋势,为铁型脱氮技术提供了理论支撑。     

栽培稻和普通野生稻居群根表铁膜形成能力的比较研究

根表铁膜形成能力反映了水稻根系氧化力的强弱。为了了解普通野生稻根系氧化力,采用水培铁胁迫试验对5个水稻品种和2个普通野生稻居群根表铁膜形成能力进行评价。结果表明:同亚洲栽培稻相比,普通野生稻拥有较高的根孔隙度,但其根表铁膜含量较低;供试植株的根孔隙度与根表铁膜含量之间没有相关性,这很可能与侧根的数量有关。     

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。     

Suppression of influenza virus infection by the orf virus isolated in Taiwan

Orf virus (ORFV), a member of parapoxvirus, is an enveloped virus with genome of double-stranded DNA. ORFV causes contagious pustular dermatitis or contagious ecthyma in sheep and goats worldwide. In general, detection of viral DNA and observing ORFV virion in tissues of afflicted animals are two methods commonly used for diagnosis of orf infection; however, isolation of the ORFV in cell culture using virus-containing tissue as inoculum is known to be difficult. In this work, the ORFV (Hoping strain) isolated in central Taiwan was successfully grown in cell culture. We further examined the biochemical characteristic of our isolate, including viral genotyping, viral mRNA and protein expression. By electron microscopy, one unique form of viral particle from ORFV infected cellular lysate was demonstrated in the negative-stained field. Moreover, immunomodulating and anti-influenza virus properties of this ORFV were investigated. ORFV stimulated human monocytes (THP-1) secreting proinflammatory cytokines IL-8 and TNF-α. And, pre-treatment of ORFV-infected cell medium prevents A549 cells from subsequent type A influenza virus (IAV) infection. Similarly, mice infected with ORFV via both intramuscular and subcutaneous routes at two days prior to IAV infection significantly decreased the replication of IAV. In summary, the results of a current study indicated our Hoping strain harbors the immune modulator property; with such a bio-adjuvanticity, we further proved that pre-exposure of ORFV protects animals from subsequent IAV infection.     

遮荫处理对铁尾矿基质臭柏实生苗快速叶绿素荧光特性的影响

【目的】通过比较分析铁尾矿基质下不同遮荫处理间臭柏实生苗叶片原初光化学反应的差异,揭示臭柏在不同光照条件下的光保护机制,从理论上解释其天然更新过程,为臭柏光胁迫的研究提供理论依据,也为臭柏在铁尾矿废弃地造林提供技术依据。【方法】以唐山迁安铁尾矿为基质,通过盆栽遮荫试验,利用快速叶绿荧光诱导动力学测定与 JIP-test数据分析方法,分别测定0,25%,50%,75%和90%5个遮荫处理下臭柏叶绿素8项荧光参数。【结果】1)全光照条件下Fo 增大,Fm 减小,而叶片光合系统量子产额和能量分配比率(φPo,Ψo和φEo)、单位面积光合机构的比活性参数(Fm,ETo/CSm和 TRo/CSm)和单位面积内反应中心的数量(RC/CSm)均最小,且各个遮荫处理组间差异均达到显著(P＜0.05)或极显著水平(P＜0.01),表明全光照条件下臭柏实生苗反应中心失活,受到光抑制,而全光照下快速叶绿素荧光诱导动力学曲线中 K 点与 J 点明显高于其他遮荫处理,而且光抑制对臭柏叶片PSⅡ的供体侧(OEC)有伤害,造成PSⅡ受体侧(Q －A )的大量积累,阻碍电子传递链向Q －A 下游传递。2)全光照条件下叶片热耗散的量子比率(φDo )和单位面积光合机构的比活性参数( DIo/CSm )均最大,且与其他遮荫处理组间差异也均达到显著(P＜0.05)或极显著水平(P＜0.01),表明全光照条件下臭柏在遭受光抑制后,通过增加天线色素的热耗散,增加非辐射能量耗散等一系列机制来保护光合机构免受过量光能的危害。3)随着遮荫率增加,φPo ,Ψo和φEo,Fm(ABS/CSm),ETo/CSm和TRo/CSm,RC/CSm随之上升,而φDo和Fo(ABS/CSo),DIo/CSm随之下降,90%遮荫处理表现出明显的光捕捉特征,50%遮荫处理 Fm ,PIABS的平均值最大,说明该遮荫条件下臭柏叶片光抑制最小,光合能力最强,其他参数在不同遮荫处理组间无明显差异( P＜0.05)。【结论】臭柏幼苗若无遮荫措施,受到光胁迫,而其通过增加非辐射能量耗散途径达到光抑制防御的机制。因此臭柏天然更新从乌柳灌丛下开始,逐渐脱离乌柳灌丛的保护,完全暴露在全光照条件下,进而实现自身的不断生长、壮大,但在废弃地上植苗造林初期尚需采取一定的遮荫措施,以提高造林成活率。     

Fluvial sediments in the Alagxa Plateau as a dust source: iron mineralogical and geochemical evidence

The Alagxa Plateau, in the margin of the northeastern Tibetan Plateau, is one of the most important dust source areas in East Asia, and the widespread sandy desert in the area is important both as a reservoir and a source of eolian silty. The northeastern margin of the Tibetan Plateau is one of the most actively-growing mountain belt on earth, and has large amounts of debris, with masses of fine grained material, which were continuously mobilized and deposited in the Alagxa Plateau by rivers, forming broad alluvial fans. It is possible that the role of fluvial sediments as a source of silty dust in the Alagxa Plateau has been underestimated. In this study, we test this hypothesis by investigating the iron mineralogical and geochemical characteristics of the fluvial sediments and the surface material of the sandy desert in the Alagxa Plateau, and comparing them with paleo-eolian dust deposits(loess) in the adjacent Chinese Loess Plateau(CLP) to investigate the possible linkages among the fluvial sediments, sandy desert and the last glacial loess of the CLP. The results show that sandy desert typically have high contents of goethite, and high ratios of goethite to hematite, similar to the fluvial sediments in the Alagxa Plateau. Based on the major element characteristics, field investigations and the results of previous studies, we found a genetic link between the silt component of the fluvial sediments and the sandy desert in the Alagxa Plateau with high value of Gt(goethite) and similarity of the Gt/(Hm(hematite)+Gt) ratio. But the silt component of the sandy desert main come from the adjacent fluvial sediments. The iron mineralogical characteristics(χ(magnetic susceptibility), χARM(anhysteretic susceptibility), SIRM(saturation isothermal remanent magnetization) and SIRM_(AF100 mT)(SIRM demagnetized at 100 mT)) of the CLP samples overlap with those of the fluvial sediments in the Alagxa Plateau, but there is a mismatch with the sandy desert samples. This suggests that the fluvial sediments are the source of a large amount of silty material which could be transported to the CLP. Therefore, we conclude that the fluvial sediment in the Alagxa Plateau is an important source of eolian silt, which is deposited in downwind region, and that this source has been previously underestimated.