岩溶地下河反硝化作用的有限性——一个碳酸盐岩管道的实验研究

反硝化作用是公认的去除水体中硝酸盐的路径,但相比于多孔介质,岩溶地下河中反硝化效果具有不确定性.为更好地认识岩溶地下河中反硝化效果,本研究利用天然碳酸盐岩管道几何模型,以乙醇为可利用电子供体(碳源),示踪了控制流速条件下管道流中反硝化作用,并辅以多孔介质流实验进行对比.反应示踪、地球化学印迹和微生物检测结果表明:当碳源缺乏时,反硝化作用没有明显启动的迹象;一旦补充了碳源,溶解氧、硝酸盐浓度和质量都出现了明显衰减,并且有中间产物亚硝酸盐产生,水体碱度增加.然而,即使在碳源充足情况下,管道流中反硝化强度却明显比多孔介质流中强度低,两者硝酸盐生物去除率分别为39.4%和大于99%,生物降解速率分别为0.113和10.8 mg·L~(-1)·h~(-1).推测其原因,一是碳酸盐岩管道内固体表面积与水体积比值低,固体吸着条件不利于微生物生长与发育,降低了硝酸盐去除率;二是管道富含的溶解氧可能延迟了反硝化作用启动,溶解氧降至3.0 mg·L~(-1)左右时硝酸盐浓度才有明显衰减.相比之下,其它环境因素如p H值和温度没有出现明显变化.该研究意义在于:岩溶管道流反硝化去除硝酸盐的潜能是存在的,但即使可利用碳源充足仍具有明显的局限性,这可能意味着岩溶地下河一旦遭受硝酸盐污染,其作为饮用水源的安全风险更大.     

气候和人类活动对典型岩溶地下河系统径流年际变化的影响

为揭示气候变化与人类活动对岩溶地下河系统年径流量的影响,以南洞地下河为研究对象,利用其1972-2014年的径流量、降水量和蒸散量数据,分析其年际变化特征。研究结果表明：研究期内径流、降水和蒸散均呈现波动减少的趋势。其中流域内径流整体以0.014亿m³/a的速度减少,降水整体以3.14 mm/a的速度减少,蒸散整体以7.94 mm/a的速度减少。通过有序聚类法和Mann-Kendall法综合确定出径流、降水的突变年份为2002年、2008年。通过累积量斜率变化率比较法,定量分解了不同时期气候与人类活动对径流变化影响的贡献率：综合考虑降水和蒸散因素,以人类活动轻微的T₁（1972-2002年）阶段为基准期,气候变化对径流减少的贡献率在T₂（2003-2008年）、T₃（2009-2014年）时期分别为-86.68%、35.92%,人类活动对径流减少的贡献率在T₂、T₃阶段分别为186.68%、64.08%。可见,人类活动是南洞地下河流域径流量年际变化的主导因素,其中生活、生产的直接耗水和土地利用/土地覆被变化影响下径流过程的变化,共同影响着径流年际变化。     

华南某金矿下游河道砷镉分布特征

对华南某金矿下游河道砷、镉分布特征进行了初步研究,在金矿下游河道沿程布设7个沉积物采样点及两个河道断面,分析了沉积物及断面土壤的砷、镉、铬、铜、镍、铅、锌含量。采用Tessier连续提取法分析沉积物中砷、镉等重金属的形态。砷含量高达10 208⁷0 621 mg/kg,镉含量达2.870 621 mg/kg,镉含量达2.8¹0.2 mg/kg。沉积物中砷、铅元素含量沿水流方向总体呈现减少趋势,铬、铜元素含量沿水流方向呈现增加趋势,镉元素含量沿水流方向先增加后减少。上游断面沉积物砷、镉等重金属浓度由河流中泓线向河岸方向增加,砷含量由16 617 mg/kg增加至53 197 mg/kg;下游断面则反之,砷含量由16 860 mg/kg减少至384mg/kg。沉积物中砷、镉等重金属元素主要以铁锰氧化态、有机结合态和残渣态的形式存在。     

北极沉积物中硫酸盐还原菌与生物地球化学要素的相关分析

对北极楚科奇海、白令海测区34个沉积物样品的硫酸盐还原菌(SRB)含量与CaCO3、Si、S、P、Cd、Fe、Ti、Pb、Hg等地球化学要素作了相关分析．同时分析了SRB与其所在沉积物粒度与底层水温间的关系．结果表明：SRB与Si、砂及底层水温为正相关；SRB与CaCO3、Fe、Ti、P、Pb、Hg、粉砂、粘土为负相关；而SRB与Cd、S的相关性因海区不同而不同．既有负相关．也有正相关．分析了这些相关状况及其原因．     

亚热带典型岩溶溪流水气界面CO2交换通量变化过程及其环境影响

具有较高水体CO_2分压(p CO_2)的岩溶地下水出露地表后常与大气形成较高的正向CO_2浓度梯度,因此评价岩溶水体水气界面CO_2交换通量对于岩溶碳循环过程研究具有重要意义.本文以广西柳州官村地下河补给的地表溪流为研究对象,详细讨论了岩溶溪流水-气界面CO_2交换通量.使用静态箱法和手持式二氧化碳测量仪GM70对脱气通量进行检测,结果表明,溪流的CO_2交换通量以脱气为主,地下河出口(G1点)脱气通量变化范围为139.48~890.84 mg·(m~2·h)~(-1),平均值为445.72mg·(m~2·h)~(-1),溪流下游(G2点)脱气通量变化范围为16.54~844.18 mg·(m~2·h)~(-1),平均值为159.81 mg·(m~2·h)~(-1),脱气通量的时空变化特征表现为雨季要大于旱季,地下河出口地区要大于下游地区.溪流CO_2脱气会对附近空气中CO_2气体碳同位素(δ~(13)C-CO_2)产生影响,使溪流附近空气中CO_2气体碳同位素(δ~(13)C-CO_2)值逐渐偏负,并表现出明显的时空变化,即δ13C-CO_2雨季偏负于旱季,G1点δ~(13)C-CO_2偏负于G2点.并且由于脱气作用的进行,溪流的水化学性质沿流程变化,表现为HCO-3沿流程逐渐降低,p H值升高,电导率降低,p CO_2沿流程递减,常见碳酸盐矿物的饱和指数SIc逐渐升高,δ~(13)C-DIC值逐渐偏正.     

喀斯特地区浅层地下水对植被退化的水文地球化学响应——以贵州荔波拉桥小流域为例

喀斯特地区植被退化的水文地球化学响应是喀斯特研究的重要内容之一,具有重要的科学和现实意义。选择贵州荔波拉桥小流域中四个不同植被类型的样地作为对象,按月采集浅层地下水(土壤水和表层泉水),对其进行水文地球化学各参数的分析。结果表明,土壤水中Ca2+、Mg2+、HCO3-、EC和pH值,表层泉水中Cl-、NO3-和SO24-等对植被退化响应敏感;而土壤水中NO3-和SO24-,表层泉水中Mg2+、NH4+、HCO3-和EC,以及土壤水和表层泉水中δ13 CDIC值则可能还受到其他过程的影响,需谨慎使用。由此可见,对于土壤层,阳离子和与土壤CO2气体浓度有关的HCO3-可能有较好的响应,而对于表层泉水,HCO3-以外的阴离子可能更敏感。     

重庆南山表层岩溶泉与地下河三氮运移及氮通量估算

岩溶区特殊的地质构造使地下水系统存在多重水流.为研究三氮在表层岩溶带水流和地下河水流中的特征和运移方式,选取城市化进程中的重庆南山老龙洞地下河流域表层岩溶泉和地下河按月采样,分析水化学特征,结合SPSS的相关性分析,认为两种水流三氮特征差异很大.表层岩溶泉三氮质量浓度月变化小,受降水、污水影响较小,NO_3~--NNH_4~+-N;地下河水三氮质量浓度月变化大,受降水、污水影响较大,旱季NH_4~+-NNO_3~--N,雨季NO_3~--NNH_4~+-N.表层岩溶泉DIN主要来源于与农业活动有关的非点源污染,在土壤、表层岩溶带中经氨化、吸附、硝化作用等过程以扩散流形式运移至出露地表.地下河DIN随管道流、扩散流运移,并以管道流为主.DIN全年有点源的工业、生活污染物经落水洞、裂隙、溶隙进入.雨季同时存在占更大比例的非点源污染物,或由降雨产生的表面坡流、壤中流、表层岩溶带水流经落水洞进入,或经深裂隙、溶隙下渗进入,硝化作用明显.流域DIN输出通量为56.05 kg·(hm~2·a)~(-1),其中NH_4~+-N、NO_3~--N分别占46.03%、52.51%;根据径流分割法估算出点源污染、非点源污染的贡献率分别为25.08%、74.92%.     

城市生活垃圾产量影响因素的路径分析——以厦门市为例

城市生活垃圾产量日益剧增,已成为制约我国城市健康和可持续发展的瓶颈.深入开展城市生活垃圾产生量的影响因素研究有助于揭示垃圾产生机制,把握其动态变化趋势,从而指导生活垃圾可持续管理及调控.因此,以厦门市为例,基于1979-2010年生活垃圾清运量及经济、生活水平、城市发展水平、社会人口学特征、自然等方面的时间序列数据,运用路径分析方法,开展了城市生活垃圾产量影响因素研究.结果表明,所构建的路径分析模型拟合优度很高,相比较简单的相关分析,很好地解释了因素与垃圾产量的因果关系;城市规模、人均可支配收入、城市化率、GDP的直接影响系数分别为0.58(p ＜0.001)、0.55(p＜0.001)、0.52(p ＜0.001)、0.51(p ＜0.001),均大于0.5,说明正影响作用很大;家庭特征直接影响系数为-0.40(p ＜0.001),为较大负影响;GDP通过旅游人次、城市规模通过家庭特征对垃圾产量有间接作用,影响系数分别为0.13(p ＜0.001)、0.31(p＜0.001);各因素总影响系数排序为城市规模(0.89,p＜0.001)＞ GDP(0.64,p ＜0.001)＞人均可支配收入(0.55,p ＜0.001)＞城市化率(0.52,p ＜0.001)＞家庭特征(-0.40,p＜0.001)＞旅游人次(0.19,p＜0.001)＞年均温度(0.09,p ＜0.001);旅游人次影响作用为中等偏弱,温度只引起生活垃圾产量的年内变动而不影响年际变化.     

滨海地区畜禽养殖户污染防治意愿影响因素及其响应机理—以盐城市为例

养殖户污染防治意愿是采取畜禽养殖污染物处理方式的基础。明确滨海地区养殖户污染防治意愿的关键因素,辨析污染防治意愿形成机理,对制定有效政策有着重要意义。以盐城市为例,基于121份调查问卷,运用结构方程分析养殖户污染防治意愿的形成机制与影响机理。结果表明：（1）个体特征、社会影响及感知、养殖户健康风险感知对于污染防治意愿有直接正向影响;（2）个体特征对养殖户环境风险感知、健康风险感知有正向影响,与社会影响及感知有共变关系,并通过这些因素间接影响养殖户污染防治意愿;（3）养殖户健康风险感知是影响滨海地区畜禽养殖污染防治意愿最主要的因素,借助路径：养殖对于人体健康影响的感知→健康风险感知→养殖户污染防治意愿可以有效提高区域养殖污染防治。     

Spatial and temporal variability of agricultural pollutants in an agricultural headwater stream within a multipond system, southeastern China

The spatial and temporal variability of nutrients and suspended solids were investigated for two years in a 1.8 km agricultural headwater stream, located by Chaohu Lake, southeastern China. The stream form was greatly modified by human activities into channelized, pond and estuary shapes. The stream could be divided into 4 channelized reaches(1.3 km), a pond reach(0.15 km) and 3 estuary reaches(0.36 km). It was found that nutrients and TSS concentrations in the stream showed temporal variability, and higher concentrations occurred in months with high precipitation and intensive agricultural activities. And, retention of total nitrogen ( TN ), nitrate ( NO3-N ),ammonium( NH4^ -N) and total suspended solids (TSS) predominantly occurred in the pond reach and estuary reaches with larger width and low current velocity. Pollutants retained in these reaches accounted for more than 50% of those retained in whole stream. The retention mostly happened in the rain-runoff events and it was 7 to 27 times than that in base flow. The results showed that the channelized reach was the most important source for pollutants release under either runoff or base flow, and its release accounted for more than 90% of whole stream release.There was a high spatial variability of nutrients retention in different channelized reaches. The channelized reach directly discharging into the pond did always retain nutrients and TSS under base flow and runoff conditions, whereas the other channelized reaches performed differently in different hydrological conditions. The high spatial and temporal variability of nutrients and TSS in the stream indicated that anthropogenic disturbance of the agricultural headwater stream, such as channelization and excavation, would be expected to decrease the capacity of nutrients retention in the stream.     

The profiles of chiral pesticides in peri-urban areas near Yangtze River: Enantioselective distribution characteristics and correlations with surface sediments

Chiral pesticides account for 30% of pesticides. Pesticides are inevitably leached into the groundwater by runoff. At the watershed level, the distribution characteristics of enantiomers in sediments collected from the river network of an agricultural area near the middle and lower reaches of the Yangtze River were tested, and their potential correlations with the physicochemical properties and microbial communities of the sediments were analyzed. The sediment pollution was serious at sites 8 and 9, with their pollution source possibly being agricultural or industrial sewage. Moreover, there were higher cumulative contents of pesticide residues at sites 4, 8, and 9. Specifically, Cycloxaprid was the most detected chiral pesticide in the study area, followed by Dinotefuran and Diclofop-methyl. Additionally, Ethiprole and Difenoconazole had strong enantioselectivity in the study area. Interestingly, the enantiomers of some chiral pesticides, such as Tebuconazole, had completely different distributions at different sites. Pearson correlation analysis showed that sediment catalase and microbial biomass carbon were important factors for enantioselectivity of chiral pesticides. The effect of sediment physicochemical properties on enantioselective distribution was achieved by influencing the microorganisms in the sediment. Furthermore, the enantioselective distribution of Tebuconazole was closely related to the genus Arenimonas. Overall, the enantioselective distribution of most of the chiral pesticides was positively correlated with the prokaryotic microbial community. This study provides empirical support for agricultural non-point source pollution caused by chiral pesticides, and also lays a research foundation for exploring the factors that affect the fate of chiral pesticides in the environment.     

中国南方喀斯特地区石灰土容重传递函数模型及影响因素研究

土壤容重(BD)数据的缺失严重影响了我国南方喀斯特地区土壤碳储量的估算,亟待利用已有数据来构建容重传递函数模型(PTFs)。本文利用南方喀斯特分布省份的石灰土土壤普查数据,首次较为系统地研究了喀斯特地区石灰土的容重传递函数模型及影响因素。研究结果表明:(1)国内外已发表的容重PTFs对中国南方喀斯特地区非地带性石灰土的适用性较差,需要进行优化或重新建立新的容重函数预测模型;(2)优化后的模型Shiri et al(2017)~*、韩光中等(2016)-a~*和韩光中等(2016)-c~*的预测精度得到明显提高;(3)基于石灰土亚类建立的PTFs具有很高的拟合度和预测精度,比优化模型更加适宜于喀斯特石灰土的土壤容重预测;(4)不同石灰土亚类容重预测的影响因素存在差异,其中土壤有机质含量是石灰土容重预测的关键因素,与各亚类土壤的BD都有很高的相关性;(5)土壤容重传递函数模型的适用性不仅与研究区域有关,同时也与研究的土壤类型有关。建议在今后喀斯特地区土壤容重预测模型研究中充分考虑地域差异性和土壤类型因素。     

Integration of chemical and biological methods: A case study of polycyclic aromatic hydrocarbons pollution monitoring in Shandong Peninsula, China

Polycyclic aromatic hydrocarbons(PAHs), as persistent toxic substances(PTS), have been widely monitored in coastal environment, including seawater and sediment. However, scientific monitoring methods, like ecological risk assessment and integrated biomarker response, still need massive researches to verify their availabilities. This study was performed in March, May, August and October of 2018 at eight sites, Yellow River estuary(S1), Guangli Port(S2), Xiaying(S3), Laizhou(S4), Inner Bay(S5), Ou...     

大亚湾拟菱形藻(Pseudon-itzschiaspp.)种群的季节变化与环境因子的关系

1997年7月至1998年6月期间，对大亚湾海域拟菱形灌种群的季节变化及其与环境因子之间的关系进行研究。高密度的拟菱形藻出现的温度、盐度范围分别在25．0－30．0℃和28．40‰～31.30‰。该水域N、Si含量丰富，P含偏低，通常情况下，P成为拟菱形藻生长的限制因子，而春季高峰期中，拟菱形藻的消退主要可能与N的迅速耗尽有关。N、Si、P三种营养盐之间比值的变化亦是影响拟菱形藻生长的重要原因，拟菱形藻高密度出现的N：P、Si：P、Si：N范围分别是6．21－32．98、59．67－119．71、3．36－17．89。     

Vertical and temporal distribution of nitrogen and phosphorus and relationship with their influencing factors in aquatic-terrestrial ecotone： a case study in Taihu Lake, China

Vertical and temporal distributions of N and P in soil solution in aquatic-terrestrial ecotone （ATE） of Taihu Lake were investigated, and the relations among N, P, ORP （oxidation reduction potential）, TOC, root system biomass and microorganism were studied. As a whole, significant declines in TN, NO3^--N, DON （dissolved organic nitrogen） and TP concentration in soil solution have occurred with increase of the depth, and reached their minima at 60 cm depth, except for NH4^＋-N, which increased with depth. The concentration of TP increased gradually from spring to winter in the topsoil, the maximum 0.08 mg/L presented in the winter while the minimum 0.03 mg/L in spring. In the deeper layer, the concentration value of TP fluctuated little. As for the NO3^--N, its seasonal variation was significant at 20 cm depth, its concentration increased gradually from spring to autumn, and decreased markedly in winter. Vertical and temporal distribution of DON is contrary to that of NO3^--N. The results also show that the variation of N and P in the percolate between adjacent layers is obviously different. The vertical variation ofTN, TP, NO3^--N, NH4^＋-N and DON is significant, of which the variation coefficient of NO3^--N along the depth reaches 100.23%, the highest; while the variation coefficient of DON is 41.14%, the smallest. The results of correlation analysis show that the concentration of nitrogen and phosphorus correlate significantly with TOC, ORP, root biomass and counts of nitrifying bacteria. Most nutrients altered much from 20 to 40 cm along the depth. However, DON changed more between 60 and 80 cm. Results show that soil of 0-60 cm depth is active rhizoplane, with strong capability to remove the nitrogen and phosphorus in ATE. It may suggest that there exists the optimum ecological efficiency in the depth of above 60 cm in reed wetland. This will be very significant for ecological restoration and reestablishment.     

Hydrogeochemical and mineralogical characteristics related to heavy metal attenuation in a stream polluted by acid mine drainage: A case study in Dabaoshan Mine, China

Dabaoshan Mine, the largest mine in south China, has been developed since the 1970s. Acid mine drainage (AMD) discharged from the mine has caused severe environmental pollution and human health problems. In this article, chemical characteristics, mineralogy of ocher precipitations and heavy metal attenuation in the AMD are discussed based on physicochemical analysis, mineral analysis, sequential extraction experiments and hydrogeochemistry. The AMD chemical characteristics were determined from the initial water composition, water-rock interactions and dissolved sulfide minerals in the mine tailings. The waters, affected and unaffected by AMD, were Ca-SO₄ and Ca-HCO₃ types, respectively. The affected water had a low pH, high SO₄^2- and high heavy metal content and oxidation as determined by the Fe²⁺/Fe³⁺ couple. Heavy metal and SO₄^2- contents of Hengshi River water decreased, while pH increased, downstream. Schwertmannite was the major mineral at the waste dump, while goethite and quartz were dominant at the tailings dam and streambed. Schwertmannite was transformed into goethite at the tailings dam and streambed. The sulfate ions of the secondary minerals changed from bidentate- to monodentate-complexes downstream. Fe-Mn oxide phases of Zn, Cd and Pb in sediments increased downstream. However, organic matter complexes of Cu in sediments increased further away from the tailings. Fe³⁺ mineral precipitates and transformations controlled the AMD water chemistry.     

半干旱地区典型POPs硫丹环境多介质迁移归趋模拟研究——以兰州河谷盆地为例

以硫丹为研究对象,利用三级多介质逸度模型,对硫丹在半干旱的兰州河谷盆地大气、水体、土壤、沉积物和植物相中的浓度分布进行模拟研究;对硫丹在研究区环境多介质问的迁移通量进行分析,确定其在环境中的主要迁移过程;并结合实际监测数据,对模型的可靠性进行验证;此外,还对除常数之外的20个模型参数进行灵敏度分析,并对较高的模型灵敏度影响因素进行不确定性分析.研究结果表明:土壤、植物和沉积物相是硫丹在兰州河谷盆地环境污染的主要储库;大气平流输入和农药施用是研究区硫丹的主要输入源,沉积物降解和大气平流输出为研究区的主要消耗和输出途径;亨利常数、辛醇-水分配系数等化合物理化性质参数,以及沉积物、土壤有机碳含量等环境参数对模型的灵敏度影响比较显著;模拟浓度与实测浓度相差在一个数量级之内,吻合较好,表明建立的三级多介质逸度模型适用于半干旱的兰州河谷盆地α-硫丹和β-硫丹的环境多介质迁移及归趋行为模拟.     

Water environmental planning and management at the watershed scale: A case study of Lake Qilu, China

Water environmental planning and management has become essential for guiding the water pollution control activities. Past water pollution control activities have been site specific, with little thought on water quality standard reaching at the watershed scale. Based on the watershed approach, a seven-step methodological framework for water environmental planning and management was developed. The framework was applied to water environmental planning and management of the Lake Qilu watershed in Yunnan Province, China. Results show that the reduction amount of total nitrogen (TN) under the plan is 1,205 tons per year so that the target of environmental capacity can be reached in 2020. Compared with traditional methods, the framework has its prevalence and could be generalized to analogous watersheds.     

南方丘陵山地农户对生态系统服务的感知及其影响因素——以湖南省慈利县为例

生态系统服务是保障乡村生态安全、环境健康以及经济可持续发展的重要基础,农户作为乡村地域生态系统与乡村经济发展的重要关联主体,其生产生活以及对生态系统服务的认知与感知变化对维护生态系统功能具有重要影响。以南方丘陵山地重点生态功能区——湖南省慈利县6个不同发展类型的农村社区为研究对象,基于农户访谈与入户调查,探究了2008—2018年农户对各类生态系统服务的多样性感知变化,采用多元线性回归方法构建农户对生态系统服务多样化感知指数模型,分析其影响因素,在此基础上提出两者协同发展的建议策略。结果表明：（1）农户对各类生态系统服务感知变化以及不同区域之间的感知均呈现差异性,农业生产主导区感知强于生态保护核心区和生态经济发展区;（2）农户对林地、农田、园地、湿地生态系统服务的多样性感知以及属性感知依次减弱;（3）自然环境、资源禀赋、个体特征等是影响农户生态系统服务属性感知的重要因素。研究结果以期为维护区域生态系统服务,提升农户福祉推进生态服务提升及乡村协同发展提供参考。     

中部地区乡村生产要素协同转型的时空格局及影响因素——以湖南岳阳为例

乡村生产要素（人—地—资本）协同转型,即劳动力转移、农地流转、资本循环协同演进,对乡村发展至关重要。本文构建了要素协同转型的理论框架,探讨影响因素的作用机制;以湖南岳阳市为例,揭示了要素转型发展水平,探究了要素协同的时空演化;从内生和外源两个维度,探讨了协同水平空间异质性的影响因素。基于要素转型会由“失配”转向“协同”的理论假说,实证发现：劳动力转移水平远高于农地流转和资本循环,三者空间分异显著;要素协同程度不高但在增强,空间集聚明显;坡度、耕地资源禀赋、距县城的距离、政府农业农村投入分别是关键的内生与外源解释因素,除距县城距离仅有正向影响外,其余因素正、负向影响并存。政策举措应因地制宜。