雷州无瓣海桑群落7种元素的生物累积和循环

在雷州市附城镇岚北人工生态恢复的 7a生无瓣海桑群落生物量调查的基础上 ,对所采集的无瓣海桑进行了植物体各组分样品的灰分和元素含量测定与循环分析 ,结果表明 :无瓣海桑植物体不同组分的灰分含量范围为 2 .2 7%～ 2 6 .4 1% ,以细根的含量最高 ,枯枝的含量最低 .植物体各组分中 7种元素质量分数范围分别为K 0 .11%～ 1.5 6 % ,Na0 .11%～ 1.6 6 % ,Ca 0 .2 0 %～ 2 .6 6 % ,Mg 0 .15 %～ 1.5 9% ,Fe 0 .0 4× 10 -3 ～ 9.6 4× 10 -3 ,Zn 0 .0 5× 10 -4～ 1.0 3× 10 -4,Cu0 .16× 10 -5～ 1.5 0× 10 -5.其加权平均的富集系数为 0 .0 5～ 9.70 ,其中Ca >K >Cu >Na >Mg>Zn >Fe .群落现存生物量中的累积储量分别为K 10 9.76gm-2 ,Ca 138.89gm-2 ,Na 86 .5 7gm-2 ,Mg 81.0 7gm-2 ,Fe 13.139gm-2 ,Zn 0 .4 83gm-2 ,Cu 0 .10 8gm-2 .群落 2 0 0 1年的元素存留累积储量分别为Ca4 1.6 8gm-2 ,K 37.2 4gm-2 ,Mg 2 7.33gm-2 ,Na2 5 .5 6gm-2 ,Fe 4 .2 75gm-2 ,Zn 0 .188gm-2 ,Cu 0 .0 39gm-2 .2 0 0 1年归还量分别为Ca 2 8.5 9gm-2 ,K 16 .83gm-2 ,Mg 12 .0 7gm-2 ,Na 11.5 8gm-2 ,Fe 0 .916gm-2 ,Zn 0 .14 1gm-2 ,Cu 0 .0 2 6gm-2 .年吸收量分别为Ca 70 .2 7gm-2 ,K 5 4 .0 7gm-2 ,Mg 39.4 0gm-2 ,Na 37.1     

Anthropogenic Calcium Particles Observed in Beijing and Qingdao, China

Analysis of individual particles collected at Beijing in northern China revealed that particles abundant in calcium (Ca) always constituted a large fraction of mineral particles in the urban atmosphere. The particles were characterized by cubic morphologies. The major mineral element in the particles was Ca and few or no other mineral elements were detected. A large number of the particles were in the range of diameter <1 μm, where common natural mineral particles were rarely detected. The contribution of the Ca particles to the volume of total mineral particles greatly exceeded that of other mineral particles during non-dust-storm periods and was comparable to that during dust-storm periods. Reagent film tests showed that particulate sulfate and nitrate formation on the Ca particles was similar to that on common mineral particles. These results indicate that a large portion of Ca in the atmospheric particulate matter in Beijing was from anthropogenic sources rather than from natural sources, and the anthropogenic Ca particles acted as a significant medium for the formation of sulfate and nitrate. Similar particles were also detected at Qingdao, a coastal city in northern China. Data of a dust storm event showed that Ca-abundant particles from East China arrived there and moved out of the continent, similarly to Asian dust storm particles, suggesting possible contributions of anthropogenic Ca even in Asian dust storm samples in the downstream areas. Therefore, Ca may not be a good indicator of Asian dust from natural sources. However, the Ca particles, due to their unique shapes and elemental compositions, may provide an indicator for the atmospheric dispersion of anthropogenic particulate matters in East Asia.     

半干半湿法脱硫灰循环利用中试试验研究

半干半湿法脱硫产生的脱硫灰中混有大量有效钙和粉煤灰 ,本文对其进行了循环利用机理分析及试验研究 ,证实脱硫灰循环大大提高了钙的利用率 ,降低了钙硫比 ,但循环倍率增加到 2倍以上时 ,脱硫效率增速变缓。脱硫灰的循环利用对降低脱硫运行费用是非常有效的。     

环境因素对菹草根和叶细胞质膜Ca2+-ATPase活性的影响

通过改变溶液温度、pH值、ATP浓度、钙浓度和培养液的钙浓度等条件,研究了菹草根和叶细胞质膜Ca2+-ATPase的活性的变化.结果表明,根细胞质膜Ca2+-ATPase的活性在pH 6.0时最高,其最适反应温度为40℃;叶细胞质膜Ca2+-ATPase在一个较宽的pH范围内具有高活性,最适反应温度为45℃;溶液中ATP浓度分别为3mmol/L和4mmol/L时菹草根和叶细胞质膜Ca2+-ATPase活性最大;无论是菹草根还是叶细胞质膜Ca2+-ATPase活性,在溶液钙浓度为10-4mol/L时都最高.在营养液中添加不同CaCl2浓度培养菹草,其根和叶细胞质膜Ca2+-ATPase活性表现出差异,根细胞质膜Ca2+-ATPase活性比叶细胞质膜Ca2+-ATPase活性高,且随营养液中钙浓度的增加,这种差异加大;当营养液中钙浓度在10mg/L(2.5×10-4 mol/L)以下时,Ca2+-ATPase活性逐渐上升,营养液中钙浓度由10mg/L增加到15mg/L,Ca2+-ATPase活性陡然下降,这与溶液钙浓度对Ca2+-ATPase活性的影响相呼应.     

Effects of exogenous Ca2+ on the membrane permeability, MDA and SH group content of Alexandrium sp. LC3 under surfactant stress

The effect of Ca^2 on the removal of Alexandrium sp. LC3 under HDTMAB stress was investigated. The results showed that thetoxic effect of HDTMAB on Alexandrium sp. LC3 was significantly reduced in the presence of Ca^2 , especially under 4 mmol/L of Ca^2 .To understand the underlying mechanism, the SH group and MDA content of the cell membrane and membrane permeability weremeasured. It was found that the SH content of cell member increased, the MDA content and membrane permeability decreased whenAlexandrium sp. was treated with Ca^2 and HDTMAB complex, compared with using HDTMAB only. The data suggested that Ca^2 mightpromote HDTMAB stress resistance of Alexandrium sp. LC3 by reducing the permeability and increasing the stability of cell membrane.     

喀斯特洞穴滴水Ca、Mg离子特征与降雨、温度相关研究——以贵州安顺石将军洞为例

为了分析洞穴滴水Ca2+、Mg2+和降雨、气温内在联系、进一步帮助解译周围地区地表环境,我们从2011年6月至2012年5月对贵州石将军洞滴水Ca2+、Mg2+等地球化学特征和周围气候进行了为期一年的监测,发现7个滴水点Ca2+、Mg2+年际变化趋势具有明显一致性,分为波动区、高值区及低值区,滴水点Mg/Ca比值与月降雨量没有明显一致性变化,但波动区,高值区及低值区均值与月降雨量具有很好的相关性,能够反应外界降雨量变化。并且研究发现,在低值区由于温度和土壤CO2的影响,造成滴水Ca2+、Mg2+在1月份突变性降低,成为年际变化的波谷期。     

稀土掺杂钨钼酸盐类荧光粉水热法合成及结构与性能的研究

利用水热法制备了A0.925（MoO4）0.5（WO4）0.5∶Dy03.＋05（A=Ca、Sr、Ba）固溶体微晶。通过X射线衍射（XRD）、扫描电镜（SEM）、荧光分析（FA）等测试手段对微晶结构、形貌和发光性能进行了表征。结果表明A0.925（MoO4）0.5（WO4）0.5∶Dy03＋.05（A=Ca、Sr、Ba）复合钨钼酸盐微晶均呈现典型的四方晶相白钨矿结构。荧光光谱中的480nm处的偶合双峰和575nm处的锐而强的黄发射峰,分别对应于稀土离子Dy3＋的4F9/2→6 H15/2和4F9/2→6 H13/2跃迁。其中具有球状颗粒（尺寸为0.7μm）形貌的Ca0.925（MoO4）0.5（WO4）0.5∶Dy03.＋05微晶的发射峰强度最强,在光学材料中具有潜在应用。     

曝气加氢氧化钙复合技术抑制底泥磷释放及对底泥微生物多样性的影响

底泥磷释放是导致水体富营养化的主要原因之一,本文通过在样泥中分别投加0、0.01和0.02 mol·L-1Ca(OH)2溶液,同时进行微臭氧曝气(0.6 g·min-1),研究了曝气加氢氧化钙复合技术抑制底泥磷释放的效果及对底泥微生物多样性的影响.结果显示,投加0.02 mol·L-1Ca(OH)2组上覆水中总磷(TP)浓度的最终值与对照组相比,抑制率达到34%;从各形态磷的角度进一步分析发现,与对照组相比,该组底泥中可溶性磷和铁磷含量分别降低了92%和60%,其最终转化为钙磷是该技术的关键.通过聚合酶链式反应-变性梯度凝胶电泳技术(PCRDGGE)研究发现,各试验组微生物相似性在65%~85%之间;Berger-Parker优势度指数、Margalef丰富度指数、Shannon多样性指数变化不明显,表明该技术不会影响底泥微生物多样性.     

Ca2+在饮用水铜绿微囊藻控制中的应用

为改善饮用水藻类的混凝去除效果,以铜绿微囊藻为研究对象,考察了单独投加Ca²⁺、Ca²⁺与PAC联用、Ca²⁺与CO₃^2-原位结晶三种方法的除藻效果,并对Ca²⁺和结晶产物CaCO₃的除藻机制进行探讨.结果表明,单独采用Ca²⁺时,Ca²⁺在低浓度下对藻细胞具有吸附电中和作用,高浓度时同时还有架桥作用,但两者均无法实现对铜绿微囊藻的去除.Ca²⁺与PAC联用,Ca²⁺可以通过吸附电中和显著提高PAC的除藻效果,最大去除率可达98.0%,同时Ca²⁺与溶解性藻源有机物（dAOM）的络合可将残余铝降低50%以上.含藻水中原位CaCO₃结晶对铜绿微囊藻的去除率最高可达83.5%,其产物为带正电荷、粒径2~4 μm左右的球型球霰石.球霰石对藻细胞的去除机制包括球霰石与藻细胞的互絮凝,以及球霰石团聚物对藻细胞的卷扫絮凝,同时球霰石还可以作为加重剂促进藻晶产物沉降分离.自来水厂采用CaCO₃原位结晶与PAC联用除藻,可望降低PAC投加量和残余铝风险,并解决CaCO₃原位结晶导致的浊度和pH偏高问题.研究成果为饮用水除藻提供了新思路.     

碱性固硫剂的固硫效果分析

本文描述了各种碱性氧化物固硫效果选择实验结果,论述了煤种,燃烧温度、钙/硫比、Fe_2O_3对固硫效果的影响。