黄河水沉淀后水质对滴灌灌水器堵塞的影响

利用2013年5月—10月和2014年7月—11月的实测数据,分析了乌海市不同功能的三个典型沉淀池(如意湖、林业湖和朝阳湖)的浊度、细菌总数、叶绿素a、总氮、总磷五项水质指标的沉淀、过滤效率,利用灌水器堵塞野外调查数据并结合堵塞物电镜扫描图片,探讨了黄河水经过平流沉淀+网式过滤组合模式处理后仍会造成灌水器堵塞的原因。结果表明:各沉淀池浊度的沉淀和过滤效率均较高,其中如意湖的沉淀效率最高,平均去除率为63%;2013年朝阳湖的过滤效率最高,为60.53%,各沉淀池水质指标的过滤效果普遍较差。黄河水经沉淀过滤后仍会造成灌水器堵塞,其主要原因与细小颗粒物和微生物形成的絮状结构有关,建议对原有沉淀、过滤措施提出改进,经一、二级沉淀后在泵房内改用叠片式砂过滤器。     

Contamination of Forest Soils in the Vicinity of the Sedimentation Pond after Zinc and Lead Ore Flotation (in the Region of Olkusz,Southern Poland)

In the technological processes of ore flotation in the non-ferrous metal industry flotation, tailings constitute up to 98% of the total of the processed material. They are stored in sedimentation ponds as fine-grained drift containing an excess of heavy metals, mainly zinc, cadmium, lead and copper. After the dehydration and drying up of the surface of sedimentation ponds, these metals are carried with dust by the wind and they are accumulated in the vicinity of the ponds in humus horizons of soils causing considerable degradation and even devastation. In this publication, we have presented the results of research on the negative influence of such a structure on the soils of an adjacent fragment of forest and its dependence on the distance from the sedimentation pond. The level of degradation of the soils under research has been assessed on the basis of changes and transformations of the morphological soil profiles, the level of alkalization and accumulation of heavy metals (Zn, Pb, Cd) in the topsoil layers and their translocation in the soil horizons. The following soils have been distinguished in the investigated area: Haplic Podzols distorted and degraded as well as Urbic Anthrosols. The acquired results have served to depict the spatial accumulation of these heavy metals in the topsoil layers. The highest accumulation of heavy metals and the degradation of the forest sites connected with it has occurred in the vicinity of a sedimentation pond drain channel. Soil remediation has been recommended in this area.     

Trends and controls of Holocene floodplain sedimentation in the Rhine catchment

Holocene floodplain sedimentation in the Rhine catchment is controlled by human and climate impacts. Intricate river behaviour modifies the fluvial response to the external impacts making cause–effect analysis difficult, especially on large spatial scales. To better understand the relative importance and interdependencies of external and internal controls, temporally resolved floodplain sedimentation rates are established using three different methods: i) floodplain storage studies on the trunk stream, ii) depth/age-analysis of overbank deposits from different parts of the catchment and iii) cumulative frequency distributions of ¹⁴C-ages from floodplain deposits from various parts of the catchment. The applied methodology strongly differs with the available temporal resolution and the size of the corresponding catchment. All three methods show a strong increase in sedimentation rate for more recent periods that can be linked to increasing human impact. Evidences for climate impacts and intricate river behaviour are less clear and hindered by insufficient temporal resolution of the currently available data.     

Characterization of acetylcholinesterase and its molecular forms in organs of five freshwater teleosts

The activity and molecular forms of acetylcholinesterase (AChE, EC 3.1.1.7) were characterized in the brain, heart, white skeletal muscle and liver of the Siberian sturgeon (Acipenser baeri), European eel (Anguilla anguilla), wels (Silurus glanis), common carp (Cyprinus carpio) and silver carp (Hypophthalmichthys molitrix), belonging in four families. The brain had the highest (between 183.2±10.6 and 1361.2±189.7 mU mg^-1 protein and between 4.7±0.4 and 23.5±2.7 U g^-1 wet tissue) and the liver the lowest (between 25.3±1.9 and 126.5±22.7 mU mg^-1 protein and between 1.0±0.1 and 4.5±0.5 U g^-1 wet tissue) activity in all these fish, with the exception of the wels, where the heart contained the smallest amount of AChE (26.2±7.5 mU mg^-1 protein and 1.2±0.3 U g^-1 wet tissue). The highest tissue AChE activity was found in the carp and lowest in the sturgeon. The solubility properties and molecular forms of AChE in the four tissues were studied by extraction in high-salt medium (1.0 M NaCl) with and without the detergent Triton X-100 (0.5%, v/v). The proportions of detergent-soluble (DS) and salt-soluble (SS) forms of AChE varied considerably from one species to another, but a general tendency could be observed: the proportion of DS AChE was generally higher in the brain (between 70.4±4.1 and 82.5±1.2%) and lower in the heart (between 12.0±2.0 and 51.3±2.3%) and skeletal muscle (between 16.0±2.0 and 64.4±0.7%). Velocity sedimentation centrifugation revealed that most tissues contained the G₄ or A₄ form. Three tissues (brain, heart, and liver) of the Siberian sturgeon contained a relatively high proportion of the G1 form (between 24.3±2.4 and 28.6±4.9%), while the skeletal muscle of the wels contained only the most complex type of AChE, i.e., A₁₂. Amongst the tissues studied, the brain and liver mostly contained amphiphilic globular forms of the G₄ type, while the heart and skeletal muscle were rich in asymmetric forms (A₄ and A₁₂). It was concluded that the differences revealed in the activities of AChE and in the distribution of its molecular forms may be connected with the variation in behavioral habits (feeding and swimming patterns), and the developmental stage of the nervous system.     

鄂尔多斯高原中部5.8～4.5 Cal kaBP气候旋回的地层记录

通过对鄂尔多斯高原现代风成砂与PJHZ剖面沉积物粒度特征的对比分析,确定了剖面中4个层位(290~210,190~160,153.5~123.5,50~40 cm)基本属于风成砂沉积。结合粒度参数、碳酸钙含量、总有机碳含量及年代序列,认为此区域在5.8~4.5 Cal kaBP存在以下沉积旋回:~5 749 Cal aBP,沉积风成砂,反映该时期风砂活动强烈,气候干燥,冬季风强盛;5 749 Cal aBP前后,沉积物为灰绿色湖相层,表明这一时期存在短暂的湖面扩展,沙漠退缩;5 749~5 370 Cal aBP,沉积风成砂,反映了湖泊的退缩和沙漠的扩展;5 370~4 895 Cal aBP,湖相沉积物,反映了流域降水量的增多;4 895~4 580 Cal aBP沉积风成砂后,4 580 Cal aBP前后又出现了短暂的湖相沉积,之后又是风砂沉积。     

Study on the Sedimentation Rule of the Particles in Debris Flow

In this paper, according to the study on a great number of experiments and data analyses, the sedimentation rule of solid particles in debris flow is set up. Three main factors that influence the particle sedimentation in debris flow were studied; the basic reasons to influence the particle sedimentation were analyzed. The particle sedimentation in debris flow could be divided into three stages,i, e. the starting stage, the quick sedimentation stage and the accumulation stage,and detailed analysis on the sedimentation process each stage was made. The liquid viscosity, particle quality and additional water pressure have an important role on the sedimentation rule of the particle in debris flow.     

崇测冰帽冰芯记录与塔克拉玛干周缘观测的相逆降水趋势——兼论大气尘埃含量对高海拔山地冰川物质平衡的贡献

对钻自西昆仑山崇测冰帽6530m处18.7m长冰芯的分析得到:尘埃含量的变化影响着崇测冰帽钻点处的物质平衡———与其它气溶胶相比,沙尘微粒是冰帽钻点处降雪的主要贡献因子;以沙尘作为冰核的降雪是钻点处降水的主导形式。与塔克拉玛干沙漠周缘地区地面观测资料比较显示:近60a来的冰芯积累量所反映出的冰帽降水量在减少,同时显示塔克拉玛干沙漠周缘地区暖季降水量在增加,而沙尘恰是连接沙漠周缘地区和附近冰川区气候变化的中介。值得注意的是,本研究对于崇测冰帽冰芯中降雪积累率与尘埃沉降通量一致降低的发现具有区域范围,甚至全球范围气候变化的意义。     

平流二沉池中计及温差影响的异重流数值模拟

【目的】在同时考虑进水与池内水的污泥质量浓度差异和温度差异的条件下,对平流式二沉池内的异重流现象进行数值模拟,重点研究异重流对池内流场及污泥沉降规律的影响,为优化沉淀池结构设计及提高沉淀池工作效率提供理论支持。【方法】选取Mixture模型和RNGκ-ε2方程紊流模型,设初始时刻二沉池内水为清水,进水为含一定质量浓度污泥的污水,并通过设置池内水与进水的不同温差模拟夏季与冬季环境,利用模拟数据分析不同时刻各工况下异重流的演变规律。【结果】池内水与进水的单纯污泥质量浓度差异会产生下异重流,小温差低温水与夏季大温差低温水进入均会导致下异重流产生,温差增大,下异重流作用更为明显;高温水进入会同时产生上异重流与下异重流,冬季温差高温水进入时上异重流起主导作用,异重流产生的旋流作用明显,对沉淀池工作效率的影响很大。【结论】温差异重流与污泥质量浓度差异重流本质均为密度差异,低温水进入增强下异重流,高温水进入削弱下异重流,温度影响会消失,污泥质量浓度差异重流作用时间更长。     

近十年来核素示踪技术在土壤侵蚀研究中的应用进展

随着核素示踪技术在土壤侵蚀研究中应用的深入,土壤侵蚀研究进入了一个快速发展阶段。本文阐述了近十年来137Cs2、10Pbex7、Be、复合示踪及REE-INAA示踪等几种主要核素示踪技术在土壤侵蚀速率、泥沙沉积速率、泥沙来源和坡面侵蚀过程等研究中的应用新进展,并对今后的研究方向和发展趋势进行了分析。     

枸杞岛海藻场两种大型海藻碎屑分解和沉降特征

岛礁水域海藻场是近岸海域典型的生态系统,大型海藻分解产生的碎屑是海藻场生态功能的重要基础。为探究大型海藻碎屑对海藻场生态功能潜在规模的贡献,本研究以枸杞岛海藻场孔石莼和舌状蜈蚣藻为对象,通过现场挂袋实验和室内静水沉降测试,分析了两种海藻碎屑的组分、粒径和沉降特征。结果显示,分解过程中舌状蜈蚣藻和孔石莼的碎屑密度均逐渐减小,且各自在不同分解时期无显著差异。舌状蜈蚣藻碎屑中有机C含量和有机N含量对密度变化影响不显著,孔石莼碎屑中有机C含量对密度没有显著影响,而有机N含量对密度有显著影响。孔石莼碎屑的δ¹³C和δ¹⁵N对其密度有显著影响,舌状蜈蚣藻碎屑的密度只受δ¹³C影响。两种海藻碎屑的密度都受木质素含量的显著影响,受纤维素含量的影响不显著。粒径是两种海藻碎屑沉降速度的决定性要素之一,研究表明,舌状蜈蚣藻大型碎屑(粒径>0.830 mm)、中型碎屑(0.380～0.830 mm)和小型碎屑(0.180～0.380mm)的沉降速度分别为0.016～0.023、0.008～0.015和0.004～0.005 m/s,孔石莼...