纳米Fe、Si降解黄褐土中PCB77

采用振荡培养实验研究了纳米Fe0、纳米Si0和纳米Fe3O4对黄褐土中PCB77的降解作用。结果表明,土壤中PCB77投加量为20 mg kg-1,仅投加纳米Fe0时,投加量为40 mg g-1,反应24 h后PCB77含量接近最低,纳米Fe0对灭菌和未灭菌土壤中的PCB77降解过程均符合一级反应动力学,反应速率常数Kobs分别为0.0057 h-1和0.0081 h-1;反应64h后,反应体系中PCB77残留率分别为68.2%,和53.2%,可见灭菌土壤较未灭菌土壤中PCB77降解效果降低。纳米双元体系能促进PCB77的降解,当纳米Si0:纳米Fe0=1∶10时,土壤中PCB77降解效果最好,反应64h后,土壤中PCB77残留率仅为53%,当纳米Fe3O4∶纳米Fe0=1∶4时,土壤中PCB77降解效果较佳,反应64h后,土壤中PCB77残留率仅为42.5%。土壤中PCB77降解产物中除联苯外未发现其他降解产物,可能是PCB77在纳米Fe0表面连续脱氯的原因造成的。     

江门市新会区耕地土壤有效性Si,Ca,Mg的空间变异特征

运用地统计学,结合GIS技术研究了江门市新会区土壤有效性Si、有效性Ca和有效性Mg3种元素含量的空间分布特征。结果表明,各变量经对数转换后符合正态分布。半方差分析的结果显示,除了有效性Ca具有强空间相关外,其余的都具有中等空间相关性。从Kriging插值结果可知,有效性硅含量在115 2 30mg/kg的面积占研究区域耕地面积的34.9% ,主要分布于研究区域的中部和东北部地区;有效性Ca的含量在>10 0 0mg/kg的面积占研究区域耕地面积的71.6 % ,主要分布在研究区域的东北、中部和西北、南部的部分地区;有效性Mg的含量在>30 0mg/kg的面积占研究区域耕地面积的2 9.8% ,主要分布于研究区域的东北部地区     

Si/As调控苗期水稻吸收、外排和转运砷的研究

通过生物模拟法,将水稻幼苗分别暴露于含有10μmol/L无机三价砷As(Ⅲ)或五价砷As(V)的营养液中12,24,48h,探究硅砷摩尔比(Si/As为0∶1,100∶1和200∶1)对苗期水稻吸收、外排、转运和累积砷的影响。结果表明,水稻暴露于含As(Ⅲ)营养液中12h,与Si/As为0∶1相比,Si/As为200∶1的处理使水稻的As(Ⅲ)吸收速率降低30.7%(P0.05),且随着暴露时间的延长,水稻对As(Ⅲ)的吸收速率逐渐降低,不同Si/As对其吸收速率的影响也减弱。处理48h,100∶1和200∶1的Si/As均降低水稻根部As(Ⅲ)向茎叶的转移系数,较Si/As为0∶1分别降低51.2%和56.9%,同时水稻地上部As(Ⅲ)含量比Si/As为0∶1的处理分别降低50.7%和67.2%;暴露在As(V)营养液中12h,Si/As为100∶1促进水稻对As(V)的吸收,增幅高达82.3%,但暴露24h,Si/As为200∶1则抑制水稻根系对As(V)的吸收,以及As(Ⅲ)的外排和As(Ⅲ)由水稻根系向茎叶的转运,降幅分别为28.0%,41.9%和39.9%。暴露48h时,Si/As为200∶1的水稻As(Ⅲ)转移系数较Si/As为100∶1的处理降低57.9%,并且处理24,48h时,Si/As为100∶1和200∶1水稻地上部As(Ⅲ)含量显著降低53.6%和75.0%,25.0%和52.8%。此外,水稻根系对As(V)的吸收与As(Ⅲ)的外排之间呈极显著正相关关系(r=0.921,P0.01),该关系不受Si/As和暴露时间的影响。无论是As(Ⅲ)或As(V)处理,在12～48h的暴露时间内,Si/As为200∶1显著抑制砷的吸收、As(Ⅲ)的外排和As(Ⅲ)在水稻体内的转运。     

不同Si/Al的氢型分子筛催化热解对生物油特性的影响

为考察对于氢型分子筛(HZSM-5)的Si/Al变化和添加量对生物质热解液化的影响,该文通过离子交换法制备HZSM-5催化剂,采用激光粒度分析仪、比表面积及孔径分析仪和X射线衍射仪对催化剂的粒度、孔隙及晶体结构等性质进行表征,并在最佳油产率温度下进行木屑的催化热解。对无催化剂和不同催化条件下得到的生物油进行气相色谱质谱联用分析,结果表明,分子筛作用下,生物油产率明显降低(最大降幅8%),含水率增加。同时,液体产物中醛类、酯类、酮类、呋喃等含氧化合物及酸含量均有所降低,提高了烃类和酚类的含量,峰面积百分比最高达到12.57%和39.36%,对催化剂催化调控改善生物油品质提供了一定的科学依据。     

Si,Fe and Mn Distributions in Rice （Oryza sativa L.） Rhizosphere of Red Earths and Paddy Soils

An experiment using rhizobox was conducted to study Si,Fe and Mn distributions in rice rhizosphere of red earths and paddy soils.It was found that Si,Fe and Mn diftributions in rhizosphere of the paddy soils were characterized by a depleted zone around root suface,beyond which the concentrations gradually rost.From lmm layer to 2mm layer the concentrations dropped and then rose again.Whereas Si and Fe in red earths showed no depleted zone but even accumulated zone around root surface.Mn showed an approximately even distribution in each layer and no depletion was found in root surface layers.This indicated that during rice (Oryza sativa L.)plantation,depletion and accumulation of Si,Fe and Mn in rhizosphere were important features of matured red earths by water culture.The distribution changes of Si,Fe and Mn in relation to soil-root interaction are also discussed.     

Interactive effects of Si and NaCl on growth,yield, photosynthesis,and ions content in strawberry (Fragaria × ananassa var Camarosa)

The effects of silicon (Si) (0, 1, and 2 mM) and sodium chloride (NaCl) salinity (0, 20, and 40 mM) on the yield, photosynthesis, and ion content in strawberry grown in hydroponics were investigated. Salinity caused a reduction in leaf area and plant biomass, regardless of Si supplement. Leaf area in Si₁Na₂₀ treatment was 37% higher than that of Si₀Na₂₀ treatment. Salinity at 20 mM concentration had a 25% yield reduction in absence of Si, corresponding to no reduction in the yield in the presence of Si compared with the Si treatment without salinity. The highest reduction of photosynthetic rate (Pn) was observed in Si₁Na₄₀ treatment; however, in the presence of Si, there was no reduction in the Pn rate at 20 mM NaCl concentration. An obvious positive relationship was found between potassium/sodium (K/Na) and Pn rate. Within each Si concentration, the increased salinity increased Na concentration in the leaf tissue. However, when Si was supplied to the salinity treatments Na concentration was significantly lower than that of the similar treatments without Si. Supplement of Si to the nutrient solution increased the Si concentration in the roots, and old and young leaves. A clear negative relationship (r² = 0.71) was found between Si and Na concentration in the leaves. Salinity (NaCl₄₀) increased the proline level 2.5-fold in the absence of Si, corresponding to no changes the proline level in the presence of 1 mM Si concentration compared with the Si treatment without salinity. The salinity (40 mM) increased the electroleakage by 50% compared with 0 mM NaCl treatment in the absence of Si supplement. Findings from this study lead to the conclusion that Si supplement to the nutrient solution ameliorated the deleterious effect of salinity on the strawberry growth; these effects were attributed to an enhanced K/Na ratio and the reduction in Na content and electroleakage ability in the leaf tissue.     

Cement Stabilization of Runoff Residuals: A Study of Stabilization/Solidification of Urban Rainfall–Runoff Residuals in Type 1 Portland Cement by XRD and 29Si NMR Analysis

Urban rainfall–runoff residuals contain metals such as Cr, Zn, Cu, As, Pb and Cd and are thus reasonable candidates for treatment using Portland cement-based solidification–stabilization (S/S). This research is a study of S/S of urban storm water runoff solid residuals in Portland cement with quicklime and sodium bentonite additives. The solidified residuals were analyzed after 28 days of hydration time using X-ray powder diffraction (XRD) and solid-state ²⁹Si nuclear magnetic resonance (NMR) spectroscopy. X-ray diffraction (XRD) results indicate that the main cement hydration products are ettringite, calcium hydroxide and hydrated calcium silicates. Zinc hydroxide and lead and zinc silicates are also present due to the reactions of the waste compounds with the cement and its hydration products. ²⁹Si NMR analysis shows that the coarse fraction of the waste apparently does not interfere with cement hydration, but the fine fraction retards silica polymerization.     

Semiquantitative determination of imogolite and Al-rich allophane (Si / Al ≃ 1 : 2) in some volcanic ash soils in San'in region by a combination of thermogravimetry-differential thermal analysis and trimethylsilylation analysis of soil clays

Abstract

A method to determine the contents of imogolite and Al-rich allophane (Sil Al ? 1 : 2) in volcanic ash soils was presented. The method is based on the (1) assessment of the presence of Al-rich allophane in clays by successsive extraction with dithionite-citrate and oxalate-oxalic acid, (2) trimethylsilylation of soil clay with a mixture of hexamethyldisiloxane, HCl, and isopropyl alcohol, and determination of the content of monomeric Si based on the trimethylsilyl derivative of monomeric orthosilicate anion by gas / liquid chromatography, (3) determination of the total content of imogolite and Al-rich allophane based on the content of monomeric Si from imogolite, (4) determination of the imogolite content by Thermogravimetry (TG )-Differential Thermal Analysis (DTA) based on the weight loss due to endothermic dehydroxylation with maximum values at ca. 386°C, (5) calculation of the Al-rich allophane content by subtracting the imogolite content from the total content of these minerals, and (6) evaluation of the imogolite and Al-rich allophane content of soil by multiplying clay content of soil and the two mineral content of clay. The trimethylsilylation analysis was found to be reproducible, and the estimated total amounts of two minerals in clays by this method were adequately approximated to those evaluated from the amount of Si (= Si_o) extracted with oxalate-oxalic acid after extraction with dithionite-citrate. The variation in the abmldance of two minerals in the soil horizons of volcanic ash soils from the San'in region indicated that this method is suitable for the profile-study of volcanic ash soils.