鲁西北地区渍涝洼地人工鱼塘─台田的环境分析

鲁西北地区是黄淮海平原中低产田渍涝洼地的主要分布区之一。在鲁西北的禹城市，利用挖鱼塘、建台田的工程措施，综合改造利用这类洼地。工程实施后，通过水盐调控，改善了洼地的环境状况。监测结果表明：洼地台田土壤含盐量降低，土壤逐渐熟化。土壤有机质大量整治前后分别为０．５８２％（１９８６年）、０．９８９％（１９８９年）．土壤中的全氮、全磷也由整冶前的０．０２％、０．１４％上升到整治后的０．０６１％和０．１５８％。土壤盐分含量逐年降低，由０．５０～０．９２％下降到０．０６～Ｏ２９％。挖鱼塘建台田的生态工程措施，使浅层地下水地表化，解决了洼地积水蒸发等形成的盐渍化问题。综合环境效应显示，洼地原有的自然状况向良性转化，达到了初步治理的目的。     

平原河网地区地表水环境保护功能区划分的研究

从地表水环境保护功能区划分工作的实践出发 ,针对复杂的水文、水质条件 ,探讨平原河网地区地表水环境保护功能区划分的工作方法和实现区划目标的对策措施。     

Palaeorunoff estimations achieved from palaeoclimatic information for the southwest part of the North China Plain: an attempt to apply a climatological approach to palaeohydrology

Palaeoclimatic scenario projecting annual temperature and annual precipitation is firstly formalized with data available and speculations for the southwest part of the North China Plain (35- 37°N, 115-119°E) during the last 25000 years. Then, with three regression equations relating annual runoff to annual precipitation and derived with data of modern hydrological and meteorological records, values of annual runoff are calculated in terms of the corresponding values of annual precipitation from this palaeoclimatic scenario for this region during this temporal interval. These results indicate that runoff is the most during 8000-3000a B.P. and the least during 25000-12000 a B. P.; runoff occurring during 12000-8000 a B.P. and during 3000-0 a B.P. is less than the one occurring during 8000-3000 a B.P. and more than the one occurring during 25000-12000 a B. P.; and the runoff occurring during 25000-12000 a B. P., 12000-8000 a B. P., and 3000-0 a B.P. is respectively 43, 46 and 66 percent of the one occurring during 8000-3000 a B.P. Values of bankfull discharge for palaeochannels of the Yellow River flowing in this region during the same interval are calculated from available estimates of slope of stream-bed of these palaeochannels with a regression equation relating bankfull discharge to slope of stream-bed and ratios of bankfull-discharge are further calculated from these values for different groups of palaeochannel formed during different time spans embraced in this interval. To conduct a cross-check, these values and ratios of bankfull-discharge are compared to the corresponding values and ratios of runoff occurring during roughly the same time spans. The same direction and similar relative magnitude of changes of the surface water occurring in this region during the last 25000 years are indicated by these comparisons.     

三江平原沼泽湿地底栖无脊椎动物群落特征

为探明现阶段三江平原沼泽湿地底栖无脊椎动物群落结构及物种多样性,于2017年春、夏、秋3个季节对6个样点开展了调查.共记录3门41科72种,以水生昆虫和腹足纲为主.平均密度为（139.68±29.13）ind./m²,季节上,底栖无脊椎动物密度表现为秋季>春季>夏季.三江平原沼泽湿地主要优势种具有一定的季节性变化,其中,西伯利亚盘螺Valvata sibirica为3个季节共有优势种.指示物种分析表明：春季指示种为Potamonectes sp.,夏季指示种为Lethocerus sp.、Gyraulus centrifugus、Erpobdellidae sp.;秋季指示种为Sgementina nitida.整体上,春季Shannon-Wiener多样性指数（H'）、均匀度指数（J）、Margalef丰富度指数（d_M）均比夏、秋季高.单因素方差分析表明,Shannon-Wiener多样性指数（F=1.480,p=0.259）、Margalef丰富度指数（F=0.056,p=0.946）、Pielou均匀性指数（F=2.038,p=0.165）均不存在季节性差异.     

不同干扰强度下三江平原湿地土壤温室气体排放对冻融作用的响应

为评估季节性冻融作用对不同干扰强度湿地温室气体产生机制的影响,采用静态箱/气相色谱法,原位观测三江平原洪河国家自然保护区内未受干扰的常年积水的小叶章湿地(undisturbed Deyeuxia angustifolia wetland,UDAW)、保护区外受人类活动干扰导致湿地含水量减少的季节性积水的小叶章湿地(disturbed Deyeuxia angustifolia wetland,DDAW)以及由小叶章湿地开垦10年以上的水稻田(rice paddy,RP)的温室气体排放通量,分析季节性冻融作用对3种湿地温室气体排放的影响特征.结果表明:3种湿地在冻融期均有CO₂和CH₄排放,且在春季冻融初期CO₂和CH₄均出现短期的高排放现象,随着冻融温度升高,温室气体排放通量均逐渐增加.其中,CO₂排放通量表现为UDAW > DDAW > RP,CH₄排放通量却表现为DDAW > RP > UDAW;DDAW的CH₄排放速率与冻融温度的相关性最高(P < 0.01,R2=0.647 5),UDAW中二者的相关性最低(P < 0.01,R2=0.424 7).相关性分析显示,DDAW和RP土壤中CO₂与CH₄的排放通量均呈正相关(P均小于0.01,R2分别为0.749 1、0.574 4),而UDAW土壤中CO₂与CH₄的排放通量表现为弱相关(P < 0.05,R2=0.303 8),可见冻融温度会影响CO₂和CH₄的排放通量.季节性冻融作用影响了3种湿地土壤N₂O的排放通量,秋季冻融期UDAW和DDAW表现为N₂O的汇,而在春季冻融期3种湿地均表现为N₂O的源,表明不同干扰湿地N₂O的排放通量对冻融作用的响应不同,但均随土壤温度的升高其排放通量不断增加.研究显示,三江平原的冻融作用降低了湿地温室气体排放,干扰强度越大,冻融作用影响越小,且秋季冻融作用大于春季.      

河北平原沧州-武强土壤地球化学异常解析

河北平原多目标区域地球化学调查在沧州-武强一带发现了以As、Cu、Zn、Fe、Mn、La、Th等元素为代表的多元素地球化学异常。本文利用地球化学方法,对该异常成因、生态环境效应等问题进行解释与评价。结果表明,特殊的沉积地质环境,即平原区低洼地内的自然吸附作用是形成大规模低缓地球化学异常的主要原因;异常对久负盛名的畅销果品沧州金丝小枣品质及油气热资源勘查的指示意义值得进一步研究。     

冻融交替处理下湿地土壤可溶性铁的动态变化研究

通过原位土柱模拟实验,对比研究了冻融交替下(-10℃冻结1d后5℃融化7d作为1个冻融周期,共5个周期,并以5℃恒温培养为对照)三江平原典型环形湿地土壤可溶性铁的动态变化.结果表明,冻融交替处理导致了环形湿地3种典型湿地土壤(毛苔草群落的腐殖质沼泽土、乌拉苔草群落的草甸沼泽土和小叶章群落的草甸白浆土)溶液中的pH和Eh在经过第1个冻融周期后大都先升高,而在后4个周期后再逐渐降低;在整个实验过程中冻融组的pH有84.4%低于对照,而Eh则有82.2%的高于对照;各土壤溶液中的可溶性铁都以Fe3+为主,而Fe3+的还原受到冻融交替处理的抑制,无论Fe2+、Fe3+或总铁(TFe)的含量大都低于对照,其中TFe从(1.25±0.16)mg·L-1减少到(0.62±0.08)mg·L-1;不同土类之间,腐殖质沼泽土的pH、Eh和可溶性铁含量变化趋势与草甸白浆土的变化趋势差异显著,处于过渡带的草甸沼泽土则在pH的变化趋势上更接近于草甸白浆土,而在Eh和可溶性铁含量的变化趋势上更接近于腐殖质沼泽土;各土类不同土层之间,冻融交替对湿地上层土壤的影响要小于深层土壤.     

三江平原典型湿地类型土壤微生物特征与土壤养分的研究

为探讨不同湿地类型土壤微生物数量和酶活性的分布特征及其与土壤养分的关系,本研究选择了三江平原洪河湿地保护区4种典型湿地类型(小叶章+沼柳湿地、小叶章湿地、毛苔草湿地和芦苇湿地)的土壤为研究对象.结果表明4种湿地类型在0~30 cm土层内:1土壤有机碳、全氮和全磷均随土层深度的增加而减少,速效钾、速效磷和速效氮则未表现出有规律的变化,且不同湿地类型土壤养分含量差异显著.2土壤微生物数量为细菌放线菌真菌,3种微生物菌落数量均随土层深度的增加而减少.土壤微生物总数量以小叶章湿地最多,毛苔草湿地最少.3土壤蔗糖酶和纤维素酶活性均随土层深度的增加而减少,而土壤过氧化氢酶活性未表现出有规律的变化.小叶章+沼柳湿地和小叶章湿地中3种酶活性显著性高于毛苔草湿地和芦苇湿地(P0.05).4相关性分析表明,土壤细菌、真菌和纤维素酶与土壤养分各指标均呈极显著或显著正相关,放线菌和蔗糖酶与速效钾、过氧化氢酶与速效钾、速效磷无显著相关性关系.因此,土壤微生物和酶活性是反映土壤养分状况的重要指标.     

FRESH GROUND WATER STORED IN AQUIFERS UNDER THE CONTINENTAL SHELF: IMPLICATIONS FROM A DEEP TEST,NANTUCKET ISLAND,MASSACHUSETTS1

ABSTRACT: A deep water-resource and stratigraphic test well near the center of Nantucket Island, about 40 miles (64 km) off the New England Coast, has encountered freshwater at greater depth than predicted by the Ghyben-Herzberg principle. An uppermost lens of fresh-water, which occupies relatively permeable glacial-outwash sand and gravel to a depth of 520 ft. (158 m), is probably in hydrodynamic equilibrium with the present level of the sea and the height of the water table. However, two zones of freshwater between 730-820 ft. (222-250 m) and 900-930 ft. (274-283 m) are anomalously deep. A third zone extending from 1150-1500 ft. (350-457 m) contains slightly salty ground water (2 to 3 parts per thousand dissolved solids). Several explanations are possible, but the most likely is that large areas of the Continental Shelf were exposed to recharge by precipitation during long periods of low sea level in Pleistocene time. After the last retreat of glacial ice, seawater rapidly drowned the shelf around Nantucket Island. Since then, about 8000 years ago, the deep freshwater zones which underlie dense clay layers have not had time to adjust to a new equilibrium. Under similar circumstances freshwater may remain trapped under extensive areas of the Continental Shelf wherever clay confining beds have not permitted saltwater to intrude rapidly to new positions of hydrodynamic equilibrium. The implications are far reaching because all continental shelfs were exposed to similar hydrologic influences during Pleistocene time.     

Biomonitoring of Lead in Atmospheric Environment of An Urban Center of the Ganga Plain, India

Monitoring of atmospheric lead from the Dalbergia sissoo treewas undertaken at Lucknow urban centre of the Ganga Plain, India.Atotal of 26 leaf samples were collected in spring, monsoon and winter seasons from 16 sampling sites and was analysed by Atomic Absorption Spectrophotometry method. Lead concentrations were low in spring season, increased in monsoon to winter seasons and range from 2.1 to 28.2 μg/g (dry wt.). This accumulative response of lead in the tree leaves is directly linked with the exposure time of automobile emission that is considered to be the predominant source for it. Highway localities show higher lead concentrations by a factor of 2 as compared to urban localities. Highest concentration was recorded at Sitapur Road (National Highway No. 24) in winter season. A linear quantitative relationship between urban air-lead levels and lead-in-the Dalbergia sissoo leaves is used to infer the qualitative assessment of present day atmospheric lead pollution. Reported results suggest a drastic reduction in mean lead concentration in Lucknow urban air from 1.32μg/m3 in 1994 to 0.19μg/m3 in 2002. Similarly, mean lead concentration in the tree leaves during winter season also dropped from 17.9 μg/g in 1994 to 8.1 μg/g in 2004. Despite of increasing urban population, urban area, vehicle population and traffic density, the introduction of unleaded-petrol (vehicular fuel) keeps lead level in the urban environment of Lucknow much lower than the past. Like Lucknow, other urban centres of the Ganga Plain are also on way to the exponential increase in pressure of urbanization. An appropriate urban public transport planning is required to provide healthy atmospheric environment for millions of people especially future young generation.