镇雄县2011-2014年期间农村饮水安全工程水质卫生监测结果分析

目的了解和掌握农村饮水安全工程水质卫生状况及其变化趋势、为改善农村饮水安全工程的水质卫生状况和预防介水性传染病提供科学依据。方法按照《云南省农村饮水安全工程水质监测技术方案》进行采样检测。结果 2011年-2014年共监测480个工程,共监测960个小水样、合格396份,合格率为41.25%,呈逐年下降的趋势(?2=55.47,p0.01);无论是出厂水与末梢水,合格率均较低无差异性(?2=0,p0.05);枯水期水质显著好于丰水期(?2=124.22,P0.01),枯水期不同年份合格率有显著差异(?2=30.47,P0.01),丰水期不同年份合格率有显著差异(?2=33.92,P0.01)。单项指标低于90%的有:总大肠菌群、耐热大肠菌群、菌落总数等指标。结论:镇雄县农村饮水安全工程以日供水规模较小的工程为主,无完全水处理工程。供水合格率呈逐年下降趋势,微生物不合格是水质合格率低的主要原因。     

山东潍坊地下水硝酸盐污染现状及δ15N溯源

采用均匀布点选取了山东潍坊居民区、粮田和蔬菜种植区等区域地下水为研究对象,分析了地下水硝态氮含量及污染来源,结果表明:潍坊地区地下水硝态氮平均含量为28.1 mg/L ,按照国家地下水质量标准(GB/T 14848-93)属于Ⅲ类水;饮用水井硝态氮平均含量为23.3 mg/L, 最高值达到了150 mg/L,对国家饮用水标准(10 mg/L)超标率高达73.5%,严重超标率达50%;不同土地利用方式下地下水硝态氮含量不同,设施蔬菜种植区最高,其次是露地蔬菜种植区, 小麦-玉米种植区地下水硝态氮含量较低,但都超过了WHO饮用水中硝酸盐的最大允许含量50 mg/L的规定(折合为硝态氮11.3 mg/L);硝酸盐与水质离子之间的相关性以及水质分析相关的派珀图分析显示地下水硝酸盐污染与氮肥施用有关;根据硝酸盐δ¹⁵N的稳定同位素溯源分析,潍坊地区地下水硝酸盐41.5%来自于化肥,14.6%来自于生活污水,其他是来自化肥、生活污水和家畜粪尿的混合污染。综上,潍坊市地下水硝酸盐污染非常严重,已经对当地居民的身体健康造成了潜在的威胁;因此,亟需从源头控制做起,减少肥料的过量投入和生活污水的随意排放,以控制硝酸盐的继续污染及改善当地水环境。     

岱海水质咸化过程中若干生态因子的变化

在1996年夏季对岱海的综合调查基础上,结合自50年代以来关于岱海的地理学、水文学和水生生物学资料,对岱海水质咸化中的若干生态因子进行了比较分析,结果表明:目前岱海pH值为933,这已经接近生物适应范围的最上限;总碱度也逐年增长,而且增长极为明显;氯离子的含量也已经远远超过了1000mg/L的极限指标。上述变化清晰地说明,岱海的水质咸化过程正在加强。同时,钙镁比率越来越失调,水的硬度也不断增加,这些变化对渔业生产十分不利。       

太平湖水库水质的理化特征

总结了1985年11月至1986年7月太平湖水库水质的理化特性,结果表明:太平湖水库水质良好,透明度高平均为321cm;pH值平均为7.4;水中溶解氧丰富;总离子量较低;水质属重碳酸盐类钙组Ⅰ型水(CⅠCa).水中主要生物营养元素氮含量较高,总氮平均为1.49mg/L,磷含量较低,总磷平均为0.012mg/L.氮、磷比为124.2:1,表明磷是该水体生物生产力的限制性营养元素。水中多数理化组分有明显的季节变化,多数理化组分在平面和垂直分布上也有差异,但差异不显着。       

三湖连江水库水化学特征

总结了1987年4月至1989年10月三湖连江水库水化学特征,季节变化及其年际变动,结果表明:该水库水质清澈,透明度平均为313cm,pH值平均为7.8,水呈中性,溶解氧丰富平均为8.81mg/L;矿化度平均为121.82mg/L,水型属重碳酸盐类,钙组Ⅱ型水(CⅡCa);水中主要营养元素氮含量高,总氮平均为1.38mg/L,磷含量低,总磷平均为0.022mg/L,氮和磷比为62.7:1,表明磷是水体生物生产力的主要限制性营养元素。多数理化组分周年中出现明显的季节变化,和在平面分布上差异显着,多数理化组分年际变化不明显。       

黄淮海平原封丘试区水体理化性状的多元分析

在封丘试区内两个最具代表性水体(曹岗湖,潘店芦苇荡)水质调查的基础上,对主要水质指标及其集合进行方差分析和聚类分析,结果表明:封丘试区水体具有典型的北方水体特征,其水质的变化主要受季节影响,水体间无甚大差别。各水体pH值偏高(年平均值为8.0—9.0),属弱碱性;硬度较大(17.54—20.63德国度),均属硬水且有逐年上升趋势;离子总量较大(860—1448mg/L);碱度(4.57—5.20me/L)和主要营养物含量(总氮1.31—2.08mg/L,总磷0.100—0.135mg/L)较高,属富营养型水体。文中指出:该试区水体水质状况较好,渔业开发潜力较大,但磷是水体生物生产力的主要限制性营养物。     

上海饮用水源地青草沙水库轮虫群落结构的特征及其环境影响因子

青草沙水库是位于长江河口的一座江心水库,是现今上海最大的水源地,作为一个半自然半人工水体,其生态系统具有特殊性,既会受到来水影响,又有自身独特性,轮虫作为最有效的水质监测生物之一,能很好地反应水库的水体现状,为水库管理提供生物学参考依据。于2014~2015年对青草沙水库轮虫群落结构的特征进行了研究,依据水库轮虫水平分布和时间分布特征,分析了该水库轮虫的种类组成、优势种、污染指示种、数量分布。结合多样性指数运用聚类分析方法分析轮虫群落结构特征,采用冗余分析方法研究轮虫和环境因子的关系。两年共发现轮虫32种,2014年为20种,优势种7种;2015年为26种,优势种2种。其中针簇多肢轮虫(Polyarthra trigla)为两年共有优势种。寡污型种类共鉴定出8种。2014年年均生物密度比2015年低,分别为(156.37±119.48)ind/L和(237.12±252.86)ind/L。2014年年均生物量比2015年高,分别为(0.1316±0.1146)mg/L和(0.1229±0.1371)mg/L。聚类分析表明,轮虫的水平分布与水库的形状、地理特征水文情况有着很大关系。冗余分析(RDA)表明,水温、溶氧、总氮、总磷、浮游植物生物密度为主要影响因子。     

氨态氮和亚硝态氮对日本沼虾血细胞数量及血蓝蛋白含量的影响

以开本沼虾Macrobrachium nipponense为材料,分别测定了其在0、2.2、4.2、8.7、17.8、36.6 mg/L氨氮暴露组和0、2.0、3.2、5.0、7.9、13.3 mg/L业硝酸盐暴露组24 h急性胁迫下,血细胞数量变化和血蓝蛋白含量变化.结果表明,在氨氮浓度为8.7 mg/L,血细胞数量显著高于对照组;随着亚硝酸盐浓度升高,血细胞数量逐渐增加.在氨氮浓度为2.2 mg/L、亚硝酸盐浓度为2.0 mg/L时,血蓝蛋白含量显著高于对照组.     

邻苯二甲酸二乙基己酯对鲤非特异性免疫的影响及遗传毒性

以水和吐温-80为对照,用5、20、80、160 mg/L的邻苯二甲酸二乙基己酯（DEHP）对鲤染毒20d,研究了DEHP对鲤非特异性免疫功能的影响及遗传毒性。结果表明: 吐温-80组与水对照组相比除红细胞总核异常率显著升高外,所测定的各项指标差异均不显著。80、160 mg/L组白细胞吞噬活力、吞噬指数,血清抗菌活力,溶菌酶活性均显著低于水对照组和吐温-80组（P0.05或P0.01）,且20 mg/L组白细胞吞噬活力、吞噬指数显著低于水对照组。与吐温-80组相比,160 mg/L组血清C3含量显著降低,5、20、80 mg/L组C3含量,5、20、80、160 mg/L组C4含量则无显著性差异。20、80、160 mg/L组C3含量,160 mg/L组C4含量显著低于水对照组（P0.05或P0.01）。160 mg/L组红细胞微核率显著高于吐温-80组,80、160 mg/L组红细胞微核率显著高于水对照组。在DEHP实验浓度范围内,红细胞核异常率、总核异常率,肝细胞DPC系数均显著高于水对照组和吐温-80组。一定浓度的DEHP对鲤具有免疫毒性和遗传毒性。       

问天湖水质监测及其治理对策

对武汉生物工程学院问天湖湖水的水质进行监测,其中氨氮0.03～0.19 mg/L,总磷0.08～1.01 mg/L,化学需氧量(COD)22.26～58.22 mg/L,溶解氧(DO)2.79～4.31 mg/L,pH 7.60～8.25。由监测结果可知,pH值在正常范围内,氨氮与DO达标,总磷与COD超标,问天湖水质污染原因主要是有机物污染及磷引起的富营养化现象,并对如何改善水质提出了相应的治理对策。     

三江平原粮食作物生产水足迹时空特征及影响因素

水足迹是评价人类活动对水资源开采和水环境污染程度的重要方法,对农作物生长过程的绿水足迹、蓝水足迹和灰水足迹进行量化和分析,可以为农业用水综合评价和用水管理提供指导。以三江平原为研究区域量化粮食作物生产水足迹的时空特征,揭示粮食生产对区域水资源的占用情况,并分析水足迹的影响因素。结果表明:(1)三江平原粮食生产水足迹总量在2005-2018年间呈显著增加趋势,其中绿水足迹、蓝水足迹和灰水足迹在水足迹总量中的占比历年平均为28%、8%和64%;(2)粮食生产水足迹空间差异明显,在地市尺度,佳木斯市水足迹最高,占三江平原总量的47%,在县区尺度,富锦市、依兰县和桦南县是水足迹热点地区;(3)只考虑蓝水足迹,粮食生产给三江平原水资源造成轻度压力,而同时考虑蓝水和灰水足迹,粮食生产给三江平原水资源造成重度压力;各地市间水资源压力有较大差异,其中佳木斯市负担了该区域将近一半的粮食产量,水资源压力最高,鹤岗市则水资源压力最低;(4)降雨量、灌溉水利用效率、化肥施用量、粮食种植结构和作物单产水平等都会影响粮食作物生产水足迹,其中蓝水足迹响应种植结构的变化最敏感,灰水足迹响应化肥施用量的变化最敏感,而水足迹总量响应作物单产水平的变化最敏感。因此,建议减少化肥施用量、提高作物单产水平和优化作物种植结构纳入区域水资源可持续管理之中。     

工业水足迹评价与应用

大规模的工业生产不但消耗了大量的水资源,同时产生了大量的工业废水,这是造成和加剧全球或区域水资源危机和水环境问题最重要的原因之一。对工业生产过程的水资源综合影响进行科学有效评估是目前资源环境管理领域研究的重要问题之一,是采取有效措施、提升工业生产的水资源利用效率和管理水平的重要前提和基础。以发展和完善工业生产过程的水资源综合影响的评价系统和方法体系为目标,基于水足迹理论,提出了工业水足迹的概念,即用以测量由某一产品、工业企业、行业或区域的工业生产过程引发的水资源利用增量的一个多维指标。以此概念为理论基础,进而首先分析了工业水足迹的内涵,包括直接工业水足迹与间接工业水足迹两部分。另外,区别于全生命周期的水足迹,工业水足迹评价是针对工业生产过程中由于工业原料、辅料、能源和水的输入,以及废水、废物与产品的输出产生的水足迹,其系统边界不包括分销零售、消费使用与废物处理等环节。其次,在确定的系统边界内构建了工业水足迹的核算框架和基础方法体系,即从生产、公共及运输3个方面收集数据、处理并核算。最后,从产品、企业、行业和区域4个层面对工业水足迹的应用及其意义进行了展望。     

On the osmotically unresponsive water compartment in cells

Differences in colligative properties (freezing point, boiling point, vapor pressure and osmotic behavior) between water in living cells and pure bulk water were investigated by re-evaluating reports of the osmotic behavior of mammalian cells. In five different animal cells, osmotically unresponsive water (OUW) values ranged from 1.1 to 2.2 g per g dry mass. Detailed analysis of human red blood cell (RBC) data indicates a major role for hemoglobin OUW-values, aggregation and packing in cell volume regulation that can be explained for the first time in relevant molecular terms.     

基于多源数据的黄土高原陆地水循环结构变化分析

近几十年间,黄土高原的水循环进程在人类活动与气候变化的影响下已产生了剧烈的变化。为加深对水循环结构变化的了解与认识,利用1982-2010年的降水、蒸散发、径流、土壤储水量和社会经济用水等数据,运用Mann-Kendall趋势检验和线性回归分析方法,对黄土高原的水量平衡进行评估,且细化了组成水循环的12种水文变量,并分析了水循环各分量的变化趋势及其结构的演化规律。由于网格化的社会经济用水数据（1982-2010年）对本研究产生了较大的时间限制,因此本文注重于探究这29年间黄土高原各水文变量的变化趋势及水循环结构的演化规律。结果表明：在自然系统中,蒸散发以1.97 mm/a的速率上升（P<0.01）,径流、降水和土壤储水量分别以1.01 mm/a（P<0.01）、0.77 mm/a和0.46 mm/a的速率下降。在社会系统中,社会经济用水以0.50 mm/a的速率上升,其中主要由于生活、制造业、发电和采矿用水分别以0.22、0.23、0.30 mm/a和0.01 mm/a的速率增加所导致。此外,灌溉和牲畜用水分别以0.25 mm/a（P<0.05）、0.01 mm/a（P<0.01）的速率减少。就水循环结构而言,多年平均蒸散发和社会经济用水占水循环的平均比例分别为80.95%、15.27%,并以每年0.16%、0.06%的速率逐渐升高。径流、土壤储水量的变化占水循环的平均比例分别为4.00%、-0.24%,并以每年0.24%（P<0.01）、0.02%的速率逐渐下降。随着社会经济的发展和人口的增加,区域水资源供需矛盾将进一步加剧,本研究对黄土高原水资源的科学调控与可持续利用有重要参考意义。     

汉江上游金水河流域森林植被对水环境的影响

以汉江上游金水河流域为研究区域,分析了流域森林植被对水环境的影响。利用年降水量、林冠截留率和不同森林类型面积的数据,计算了金水河流域森林生态系统的水源涵养量,分析了流域森林植被对水量的影响;采用监测的方法,分别对金水河流域阔叶林森林生态系统的大气降水、枯落物层、土壤层和出口河水的水质进行了比较分析,探讨流域森林植被对水质的影响。结果表明,(1)金水河流域森林生态系统的水源年涵养总量为466.79×106m3,(2)流域阔叶林森林生态系统能够调节pH值,缓解大气降水的酸性环境;降低了大气降水中TDS、CODMn、HCO3、SO4、Cl、NO3、NH4-N、NO3-N、PO4-P、TDP、As、Ba、Cr、Na、Pb、Fe、K、Mn、V和Zn的含量,净化了水质。(3)根据各贮水层的水质分析,推断了河水中各物质的不同来源。研究为南水北调中线工程水源地的管理和建设提供了参考。     

The dielectric method of investigating bound water in biological material: An appraisal of the technique

Three independent dielectric methods for the measurement of water of hydration (bound water) in a biological material are described and discussed comparatively. For well-defined aqueous solutions of biological molecules, hydration can be obtained from direct observations made on the δ dispersion or from measurement of the dielectric values of the β dispersion. For whole tissue, however, neither of these two methods is applicable, and to deduce the hydration, it is necessary to use the third technique in which the volume of the hydrated biological particle is obtained by measuring the effect of it on the known dielectric properties of pure water. The hydration can then be calculated by deducting the volume of the anhydrous particle from the experimentally determined volume of the hydrated particle. Owing to possible systemmatic errors the uncertainty in the absolute hydration value associated with this technique is rather larger than that obtained with the other two dielectric methods. For studying the differences between hydration in similar tissues, however, this objection disappears.     

植物根系吸水过程中根系水流阻力的变化特征

以植物根系吸水的人工模拟试验所测得的数据为依据,运用水流的电模拟原理,定理分析了不同土壤水分水平处理下植物根系吸水过程中根系水流阻力各主要分量的大小、变化规律及其相对重要性．结果表明,在同一水分水平处理中,植物根内木质部传导阻力（Ｒｃ）随生长时间的推移而减小,随土层深度的加深而增大,土根接触阻力（Ｒｓｒ）、植物根系吸收阻力（Ｒｒ）随生长时间表现出先下降后上升阶段的动态变化特征;在不同水分水平处理中,Ｒｃ、Ｒｓｒ、Ｒｒ均随土壤湿度减小而大幅度增大;在植物根系水流阻力各分量中,Ｒｒ占根系水流阻力的比例为５５％～９６％,Ｒｓｒ约占根系水流阻力的４％～４５％,而Ｒｃ仅占根系水流阻力的７×１０－６,故Ｒｒ是决定植物根系吸水速率的重要因素     

Impact of acid mine-drainage from abandoned spoils on the chemistry of an intermittent stream in the arid Southwest

Drainage from an orphaned copper mine (Sheldon Mine Complex) contributes highly mineralized, acidic waters to Lynx Creek, a small intermittent, arid-climate stream. This results in localized elevation of major cations, silica, sulfate, and heavy metals (Cu, Fe, Mn, Zn), depression in pH, and complete neutralization of bicarbonate alkalinity. Levels of chloride, nitrogen and phosphorus are unaffected by mine-drainage. During stable flow, water quality of the creek improves downstream through precipitation of metal salts, dilution by less mineralized tributaries, and additional buffering from the creek channel and tributaries. Climatic aridity, via high evaporation, concentrates and precipitates metal salts during summertime periods of low flow. Creek sediments thus contain large amounts of heavy metals and phosphorus that are transported downstream in suspended particulates during spates. This reflects an annual cycle of temporary creek-bed storage followed by episodic mobilization toward Lynx Lake, a downstream reservoir. Although the influence of mine drainage is not overtly apparent in the dissolved chemistry of the Lake, high concentrations of metals and phosphorus occur in lake sediments.Represents a portion of a thesis by A. J. L. III submitted in partial fulfillment of the requirements of a M.S. Degree in Botany, Arizona State University.     

Longitudinal and temporal trends in the water chemistry of the North Branch of the Moose River

Surface water acidification is potentially a problem in regions with low ionic strength drainage waters. Atmospheric deposition of sulfuric acid has generally been implicated as the causative agent of this problem, although other sources of acidity may contribute. The Adirondack region of New York State is an area with acid-sensitive surface waters and an abundance of acidic lakes. The intent of this study was to evaluate the processes regulating the acid/base chemistry of a series of lakes draining a large heterogeneous watershed in the Adirondack region of New York.The study site, the North Branch of the Moose River, is heterogeneous in its soil and geological characteristics. This variability was reflected through differences in water chemistry that occurred within the basin. The northern headwaters generally drain subcatchments with shallow, acidic soils. The resulting water chemistry was acidic (equivalence of acidic anions exceeded equivalence of basic cations) with high concentrations of Al and dissolved organic carbon (DOC). As this water migrated through a large lake (Big Moose Lake) with a moderate hydrologic retention time (0.5 yr), considerable loss of DOC was evident.As acidic water was transported through the drainage area, it mixed with waters that were enriched in concentrations of basic cations from the eastern subbasins. As a result, there was a successive increase in the acid neutralizing capacity (ANC) and a decrease in Al concentrations as water migrated from the northern reaches to the outlet of the watershed.In addition to these general trends, short-term changes in water chemistry were evident. During low flow summer periods concentrations of basic cations were elevated, while concentrations of SO ₄ ^2– and NO ₃ ^– were relatively low. These conditions resulted in less acidic waters (higher ANC) with relatively low concentrations of Al. During high flow winter/spring conditions, elevated concentrations of SO ₄ ^2– and NO ₃ ^– were evident, while concentrations of basic cations were reduced resulting in low pH (low ANC) waters with high concentrations of Al.Variability in the processes regulating the pH buffering of waters was apparent through these short-term changes in water chemistry. In the northern subbasin short-term fluctuations in ANC were minimal because of the buffering of Al under low pH conditions. Seasonal changes in the ANC were more pronounced in the eastern subbasin because of the predominance of inorganic carbon buffering in the circumneutral pH waters.Lakes in the west-central Adirondacks have characteristically short hydraulic residence times and elevated nitric acid inputs. As a result these waters may be more susceptible to surface water acidification than other acid-sensitive lake districts in eastern North America. Given the apparent interregional differences, extrapolation of chemical trends in the Adirondacks to other areas may be tenuous.     

Comparative Studies on Water Relations and Xeromorphic Structures of Some Plant Species in the Middle Part of the Desert Zone in China

The mean value of leaf water potential (LWP) of the mesophytes, the less-succulent xerophytes and the succulent xerephytes was –13.5, –18.09 and –26.09 bars respectively. The bound water content (BWC), and the ratio of bound water content to free water content (B/E ratio) for the succulent xerophytes (174.0% and 4.8) were higher than those for the mesophytes (52.5% and 0.37) and the less-succulent xerophytes (76.8% and 1.0). The transpiration rate of the mesophytes, less-succulent xerophytes and succulent xerophytes was 1146.5, 866.3 and 422.8 mg/g. fw. h respectively. The water holding capacity (WHC) of the succulent xerophytes was the strongest among those of the three types, while that of the mesophytes was the weakest. The xerophytes, both the succulent and the less-succulent, have the following xeromorphic structures: thick cuticle, sundan stomata, dense epidermal hairs, well-developed palisade tissue and degenerated spongy tissue, the high ratio of palisade tissue to spongy tissue, and equilateral leaves. Besides, succulent xerophytes possess other xeromorphic structures: thick leaves, well-developed water storing tissue, high ratio of water tissue to leaf thickness, and the succulent leaves. The mesophytes exhibit the following mesophilous structures, thin cuticle, levelling or arching up stomata, low ratio of palisade tissue to spongy tissue, and back-belly leaves.