Distribution characteristics of phosphorus forms in the sand-dust and the desert particles in Inner Mongolia and its environmental significance

根据我国中路沙尘暴的影响范围和移动路径,应用颗粒物中磷的连续浸提技术,选择研究了8个站位的颗粒物样品中磷的赋存形态和分布特征.研究结果表明,各粒级样品中无机磷（IP）含量范围在300.16—1916.99μg.g-1,占总磷（TP）比率86.11%—99.84%,TP含量主要受IP控制,有机磷（POrg）含量远低于IP,彼此之间表现为负相关关系;沙尘粒子Y1—Y4（呼和浩特,2005年—2010年沙尘暴期间收集）的TP、IP、生物可交换磷（BP）和可交换态磷（Pex）含量远高于沙尘暴源地及沿途地区地表颗粒物,这与沙尘暴源地及影响区域磷污染状况及地质环境条件关系密切;粒径小于57μm的颗粒物样品的TP、IP、PCa含量均高于自然粒径颗粒物样品.     

Characterization of soil low-molecular-weight organic acids in the Karst rocky desertification region of Guizhou Province, China

Soil low-molecular-weight (LMW) organic acids play important roles in the soil-forming process and the cycling of nutrients in Karst regions. In this study, we quantified the contents of LMW organic acids (including lactate, acetate, formate, malate, and oxalate) in soil solution over the Karst region of Guizhou Province, China using ion chromatography. The concentration of total LMW organic acids in topsoil solution ranged from 0.358 to 1.823 μmol·g^-1, with an average of 0.912 μmol·g^-1. The mean concentrations of lactate, acetate, formate, malate, and oxalate were 0.212±0.089, 0.302±0.228, 0.301±0.214, 0.014±0.018 and 0.086±0.118 μmol·g^-1, respectively. There were also significant difference in the contents of these acids among four phases of rocky desertification, and their concentrations decreased with the aggravation of rocky desertification. The concentrations of the LMW organic acids were significantly positive correlated each other. Significant positive correlations were also observed among individual LMW organic acids in soil solution, and between them and soil available P, available K, exchangeable Ca, respectively. Furthermore, the concentrations of LMW organic acids were significantly positively correlated with inorganic anions (chlorides, nitrates, and sulfates) in Karst topsoil solution. Therefore, the concentrations of soil LMW organic acids might be one of driving force in the Karst rock desertification process in Guizhou Province.     

Optimal locations of monitoring stations in water distribution systems under multiple demand patterns: a flaw of demand coverage method and modification

A flaw of demand coverage method in solving optimal monitoring stations problem under multiple demand patterns was identified in this paper. In the demand coverage method, the demand coverage of each set of monitoring stations is calculated by accumulating their demand coverage under each demand pattern, and the impact of temporal distribution between different time periods or demand patterns is ignored. This could lead to miscalculation of the optimal locations of the monitoring stations. To overcome this flaw, this paper presents a Demand Coverage Index (DCI) based method. The optimization considers extended period unsteady hydraulics due to the change of nodal demands with time. The method is cast in a genetic algorithm framework for integration with Environmental Protection Agency Net (EPANET) and is demonstrated through example applications. Results show that the set of optimal locations of monitoring stations obtained using the DCI method can represent the water quality of water distribution systems under multiple demand patterns better than the one obtained using previous methods.     

石家庄地区雾霾天气下云滴和云凝结核的分布特征

2009年5~10月在石家庄地区对雾霾天气下的近地面到高空的云雾滴和云凝结核(CCN)进行了7架次飞机探测.利用PMS云粒子测量仪器、机载温湿仪和连续气流纵向热梯度云凝结核仪获得的云雾粒子和云凝结核(CCN)探测资料,分析了层积云(Sc)和高积云(Ac)中云粒子浓度、液态含水量、粒子算术平均直径和粒子有效平均直径的垂直分布特征;分析了CCN垂直和水平分布特征以及谱分布.结果表明雾霾天气状况下,云滴数浓度在102个/cm3量级上.高云粒子粒径总体大于低云粒子.云含水量平均值范围为0.03~0.14g/m3;地面到600 m高度内, CCN值的平均值为3034cm-3(过饱和度S=0.3%).对CCN的活化谱进行拟合表明石家庄属于典型大陆性核谱,云对CCN有消耗作用,逆温层的存在使得该区CCN浓度累积增加.     

洋河水库微囊藻空间分布特征及其影响因素分析

通过野外调查及现场风速实时监测,对2010年夏季我国河北洋河水库微囊藻的空间分布特征及其影响因素进行了研究.结果表明,在水平空间上,西洋河口(主要入湖河口)微囊藻细胞密度最高,库心、北库心、坝前西、东洋河口等位置次之,坝前东(取水口)处微囊藻细胞密度最低,整体呈由水库西北向东南方向降低的趋势.Pearson相关性检验表明,洋河水库微囊藻细胞密度与ρ(TP)显著相关(P<0.05),但与ρ(DTP)、ρ(TN)及ρ(NO3--N)相关性不显著(P>0.05).风场分析表明,洋河水库水华发生季节东南风风频明显大于西北风,说明洋河水库微囊藻水平空间分布主要受入湖河流氮、磷污染及风场分布共同影响.西洋河口和库心的微囊藻昼夜垂向分布特征表现为早晨主要集中在水体的表层(10 cm),中午主要分布在水体0～3.5 m的水层,而傍晚时则可能下沉至底层,昼夜变化规律明显,并且其垂向分布特征主要受藻细胞的光合作用和风浪的混匀作用共同影响.      

2006─2010年环保重点城市主要污染物浓度变化特征

利用2006─2010年全国环保重点城市的空气质量日报数据,分析了大气ρ(SO2)、ρ(NO2)和ρ(PM10)的变化特征. 结果表明:从年际变化看,ρ(SO2)和ρ(PM10)呈下降趋势,ρ(NO2)变化不显著.从季节变化看,ρ(SO2)、ρ(NO2)和ρ(PM10)均呈冬季高、夏季低的特征.从浓度谱分布看,全国大气中ρ(SO2)、ρ(NO2)和ρ(PM10)分别集中在0～0.150、0～0.100和0～0.250 mg/m3范围内,ρ(SO2)和ρ(PM10)谱峰区间逐渐向低浓度范围偏移,高浓度事件逐渐减少,表明SO2和PM10污染得到较明显的控制,而ρ(NO2)谱峰变化不大.从浓度变化看,山西ρ(SO2)、ρ(NO2)和ρ(PM10)下降最明显,年变化率分别为-11.2、-3.6和-14.2 μg/m3;青海ρ(SO2)、山东ρ(NO2)和ρ(PM10)的上升趋势最明显,年变化率分别为4.4、2.7和4.5 μg/m3.      

原子荧光冷汞法测定地表水中的汞

建立原子荧光冷汞法测定地表水中的汞,通过实验及查阅相关资料对部分实验条件,如仪器的负高压和灯电流、屏蔽气和载气的流量、硼氢化钾和氢氧化钠的浓度、酸及其浓度等进行了优化。在最佳实验条件下汞的检出限为0.019μg/L,相关系数r>0.999,加标回收率为93.7%～106.4%,相对标准偏差0.79%～3.59%。实验结果表明:原子荧光冷汞法测定地表水中的汞具有简便、快速、清洁、高效、安全等优点,灵敏度高、精确度和准确度好、检出限低,是测定地表水中汞含量的有效方法。     

中国大气NH3和NOx排放的时空分布特征

根据我国不同氨源的数量、燃料消费量和相应的氨与氮氧化物排放因子,计算了我国大陆地区1995~2004年历年的氨(NH3)排放量与1985~2005年历年的氮氧化物(NOx)排放量,在此基础上模拟了2006~2010年的NOx排放量,并分析了NH3和NOx排放强度的空间分布.结果表明:2004年,我国NH3排放量为12.0Tg,比1995年的10.6Tg增加了大约13.2%;2004年的NOx排放量为20.6Tg,比1995年的12.2Tg增加了大约68.9%,比1985年的6.2Tg增加了大约2.3倍.在1996年以前,我国NH3和NOx的排放量基本相当,但是此后NH3的年排放量在经历了1997~1999年的下降之后,变化比较平稳,而NOx的排放量自2000年之后呈逐年迅速增加的趋势.2004年全国NH3的排放总量中,畜禽排泄、氮肥施用、人类粪便、氮肥与合成氨生产的贡献率分别为69.2%、15.2%、13.9%和1.9%;2004年全国NOx的排放总量中,由于受到我国能源消费结构的制约,煤炭来源的NOx占到了排放总量的77.4%.NH3和NOx的排放强度都具有明显的空间差异,表现在中东部地区的排放强度明显高于西部地区,这与中东部地区人口多、能源消费量大以及畜禽养殖数量大有关.     

山地城市排水管网特细颗粒物特性及变化规律

对山地城市排水管网中特细颗粒物的粒径分布特征及变化规律、Zeta电位分布特征及变化规律和ρ(SS)的变化规律进行研究,同时对相关水化学参数(如电导率、pH)的变化规律进行了分析.结果表明:特细颗粒物的平均粒径、Zeta电位、ρ(SS)和电导率分别为21.04～73.53μm、-20.83～-11.15 mV、106～492 mg/L和973～2 445μS/cm,其统计平均值分别为(43.74±14.12)μm、(-17.95±1.88)mV、(233±90)mg/L和(1 343±331)μS/cm;pH为7.25～7.63.工业废水的排入对排水管网特细颗粒物的粒径分布特征、Zeta电位分布特征以及电导率有显著的影响并呈现出一定的规律性;传统沉砂池对进水中特细颗粒物的去除能力相当有限,特细颗粒物会直接进入生物处理系统.      

Spatial variability in soil water and salinity in Tamarix community in a semiarid saline region of the upper Yellow River北大核心CSCD

Tamarix is widely distributed in semiarid saline regions of the upper Yellow River. The community of Tamarix affects the spatial distribution of soil water and salinity. It is important to explore the dynamic response relationship of Tamarix community and spatial distribution of soil water and salinity in order to evaluate the effects of vegetation community construction and ecological restoration in this region. The natural Tamarix community in the secondary saline-alkali land of the Ningxia Yellow River Irrigation Area was investigated in July 2016. Classical statistics and geostatistics were used to analyze the spatial distribution characteristics of soil water and salinity. The results showed that the soil water content was relatively low (1.98%-7.55%), whereas the soil salinity was high (average conductivity 10.28-25.38 mS/cm) in the study area. The variability coefficient range of soil water and salinity was 36.1%-83.7%, both with moderate variations. Furthermore, the variation degree of soil salinity decreased with the increase in soil depth. The soil water and salinity had obvious spatial structure characteristics, which was mainly affected by structural factors or structural factors associated with stochastic factors. The coefficients of nugget were 0.04%-49.88%, indicating the strong spatial correlation. The spatial distribution of soil water and salinity in Tamarix community showed a patchy pattern; the soil water and salinity distribution in the areas with high Tamarix growing density were considerably high. The correlation analysis showed that there was a positive correlation between soil water and salinity in the study area. In conclusion, soil water and salinity restrict the distribution and growth of Tamarix. Furthermore, the distribution and growth of Tamarix enhanced the spatial variability of soil water and salinity. Keywords. © 2018 Science Press. All rights reserved.