Oxygen depletion and phosphorus release following flooding of a cultivated wetland area in Denmark     

Nina L. Grunth  Louise Askaer  Bo Elberling 《Geografisk tidskrift / udgivet af Bestyrelsen for Det Kongelige danske geografiske selskab》2013,113(2):17-25

Geografisk Tidsskrift, Danish Journal of Geography 108(2):17–25, 2008

The rewetting of altered wetlands is becoming increasingly widespread. When flooding cultivated soils, the oxygen (O₂) availability is reduced, subsequently, ferric hydroxides can dissolve and associated inorganic phosphorus (P) will be mobilized. This study shows the temporal and spatial dynamics of O₂ depletion following flooding using planar optodes and the subsequent release of Fe and P in two depth intervals in an experimental column set-up. The column was kept flooded for 48 days and thereafter partly drained and flooded again. Results document that large amounts of P (0.2 t P ha-¹) have accumulated in the present plough-layer (Ap) during the last 22 years, which represent roughly 15% of the present inorganic P stock in the Ap. As a result of flooding, fully anoxic conditions were observed within 3 days (within 10 h in Ap) and concentrations of dissolved Fe and P in the soil solution increased simultaneously after 7 days of flooding. Thus, P reaction kinetics was markedly delayed as compared to O₂ availability. P concentrations in soil water afterflooding (up to 0.15 mg L^?1) accounted for only 0.034% of the inorganic P stock in the Ap which is a significantly smaller fraction of the potential P-release as compared to previous investigations.

This is considered a result of only a minor fraction of the total inorganic P being directly associated with ferric hydroxides and thereby sensitive to short-term anoxic conditions as well as differences in the methodology used in this study (soil/water ratio). Finally, reactions releasing Fe and P were noted to be partly reversible upon draining.  相似文献   

The Hydrologic Importance of Small- and Medium-Sized Dams: Examples from Texas     

Anne Chin  Laura R. Laurencio  Adriana E. Martinez 《The Professional geographer》2013,65(2):238-251

Studies of the effects of dams have emphasized large and very large dams; less well understood are the impacts caused by smaller dams. Using Texas as an example area, this article highlights the role of small- and medium-sized dams in affecting the surface hydrology of river systems. Analysis of data from the National Inventory of Dams (NID) in a geographic information system showed that small and medium dams comprise about 97 percent of the dams registered in Texas. A small-or medium-sized dam is found approximately every 100 km² of area and about 120 km of river length. Different from large dams, which affect water storage the most, the major impact of these smaller dams is fragmentation of river landscapes. Analysis of data for dams extracted from digital orthoquads and for water bodies from the National Hydrography Dataset indicates that the extent of river fragmentation is likely greater than that suggested by data from the NID, because the NID underrepresents the smaller dams. Such extent of river fragmentation can degrade stream habitats and pose barriers to the migration of aquatic species and transport of sediment. Because small and medium dams are largely built for fire protection and stock ponds, mitigating the impacts associated with these dams likely involves working with the private individuals who own them.  相似文献   

广东流沙湾网箱养鱼区水体氮磷的时空变化及负荷估算     

周志诚  申玉春  薛海波 《广东海洋大学学报》2014,(3):65-69

研究流沙湾网箱养鱼区水体氮、磷含量的月变化和水平分布,并运用质量平衡方程估算其氮、磷负荷。结果表明:总氮变化在0.212~0.892 mg/L之间,平均0.498 mg/L;总磷变化在0.009~0.036 mg/L之间,平均0.020mg/L;氮磷比变化在23.6~26.1之间,平均为25。在5-9月,氮、磷含量变化呈逐渐增加趋势,到9月达到最大,10月又减少。网箱内部氮、磷的含量高于网箱外部,并随着与网箱距离的增大而逐渐减小。红鳍笛鲷(Lutjanus argentimaculatus)、紫红笛鲷(Trachinotus ovatus)和卵形鲳鲹(Lutjanus erythopterus)全鱼的氮质量分数平均为2.42%,磷质量分数平均为0.26%,饵料系数为6.67,流沙湾网箱养鱼养殖期产生的氮、磷负荷平均分别为135.8和19.4 kg/t。  相似文献   

一次雾霾过程中气象因子与细颗粒物浓度关系的研究   总被引：1，自引：0，他引：1  

杨晓亮  杨敏 《干旱气象》2014,(5)

利用常规气象观测资料及逐小时地面自动气象观测和环境监测部门的PM2．5浓度等资料,对2014年1月15～19日河北省持续雾霾天气期间气象因子与PM2．5浓度的关系进行统计分析。结果表明,PM2．5是造成霾阶段水平能见度下降的主要因素,相对湿度在40％～60％之间时,能见度与PM2．5浓度相关性最好,随着相对湿度的增大,PM2．5浓度对能见度的作用呈减小趋势;雾阶段能见度与相对湿度的相关性明显好于PM2．5浓度值。西北大风对河北PM2．5浓度的平均清除率在94．3％,去除时间平均为3．7 h,可使PM2．5空气质量分指数达到优或良的等级,降雪对PM2．5浓度的清除作用明显小于大风,很难将PM2．5空气质量分指数降到优或良。  相似文献   

Passive seismic data primary estimation and noise removal via focal‐denoising closed‐loop surface‐related multiple elimination based on 3D L1‐norm sparse inversion     

Tiexing Wang  Deli Wang  Jing Sun  Bin Hu 《Geophysical Prospecting》2021,69(1):122-138

Passive seismic has recently attracted a great deal of attention because non‐artificial source is used in subsurface imaging. The utilization of passive source is low cost compared with artificial‐source exploration. In general, constructing virtual shot gathers by using cross‐correlation is a preliminary step in passive seismic data processing, which provides the basis for applying conventional seismic processing methods. However, the subsurface structure is not uniformly illuminated by passive sources, which leads to that the ray path of passive seismic does not fit the hyperbolic hypothesis. Thereby, travel time is incorrect in the virtual shot gathers. Besides, the cross‐correlation results are contaminated by incoherent noise since the passive sources are always natural. Such noise is kinematically similar to seismic events and challenging to be attenuated, which will inevitably reduce the accuracy in the subsequent process. Although primary estimation for transient‐source seismic data has already been proposed, it is not feasible to noise‐source seismic data due to the incoherent noise. To overcome the above problems, we proposed to combine focal transform and local similarity into a highly integrated operator and then added it into the closed‐loop surface‐related multiple elimination based on the 3D L1‐norm sparse inversion framework. Results proved that the method was capable of reliably estimating noise‐free primaries and correcting travel time at far offsets for a foresaid virtual shot gathers in a simultaneous closed‐loop inversion manner.  相似文献   

Nutrient fluxes at the river basin scale. I: the PolFlow model     

M. J. M. de Wit 《水文研究》2001,15(5):743-759

Human activity has resulted in increased nutrient levels in rivers and coastal seas all over Europe. Models that can describe nutrient fluxes from pollution sources to river outlets may help policy makers to select the most effective source control measures to achieve a reduction of nutrient levels in rivers and coastal seas. Part I of this paper describes the development of such a model: PolFlow. PolFlow was specially designed for operation at the river basin scale and is here applied to model 5‐year average nitrogen and phosphorus fluxes in two European river basins (Rhine and Elbe) covering the period 1970–1995. Part II reports an error analysis and model evaluation, and compares PolFlow to simpler alternative models. Copyright © 2001 John Wiley & Sons, Ltd.  相似文献   

Performance of wuxi WWTP in china     

WANG Lin  WANG Li  JIANG YifengOcean University of China 《中国海洋大学学报(英文版)》2003,2(2):224-229

In Wuxi Wastewater Treatment Plant, the Anaerobic, anoxic and oxic (A2/O) process was employed to remove the nitrogen and phosphorus, which exhibited the positive results of the high removal efficiency for phosphorus with a range of 67.7% to 89.9% and an average value of 78.0. The effluent of phosphorus met the national discharge standard. The removal of TN was effected by both BOD variation of influent and wastewater temperature. TN removal was in the range of 28.5% to 55.8% with an average value of 39.4%. The energy cost was 0.15 kWh(m3d)-1 or 1.35 kWh(kgBOD·d)-1. The annual average sludge production was 46.3 m3d-1, the annual average dosage for the dewatering was 40 kgd-1.  相似文献   

重铬酸钾容量法测定铁中SnCl2加入超量的处理方法     

李军  董小平 《安徽地质》2001,11(1):71-73

重铬酸钾容量法测铁中,二氯化锡超量产生黑色汞沉淀,严重影响测定。利用空气氧化作用,无须添加任何试剂,在8-12min内解除汞的影响,较“弃之重来”的传统做法省时省力,用于铁矿样测定获满意结果,  相似文献   

A one‐year study of the Rostherne Mere ecosystem: seasonal dynamics of water chemistry,plankton, internal nutrient release,and implications for long‐term trophic status and overall functioning of the lake     

Vladimir Krivtsov  David Sigee  Edward Bellinger 《水文研究》2001,15(8):1489-1506

A study of Rostherne Mere (Cheshire, UK) was undertaken to reveal relationships among various ecosystem components and assess the progress in lake recovery following sewage diversion. An intensive monitoring programme included measurements of dissolved oxygen, T, pH, electric conductivity, K, Mg, Ca, Si, N and P species, Secchi depth, suspended solids, chlorophyll‐a, phyto‐ and zooplankton counts. Recorded changes and the results of correlation analysis broadly confirmed to the classic limnoecological theory and allowed detailed interpretation of the dynamics observed. The Si level was used to estimate the amount of diatom detritus produced in spring. Chemical profiles were used to estimate the amount of nutrients accumulated in the hypolimnion during the stratified period. These estimates were compared with simulations made using the model of exponential decay, which showed a good performance in the case of Si but considerable underestimation in the case of P. The differences between the values simulated by the model and estimates based on field observations resulted from the additional P release from the sediments. This release could have been stimulated by a combination of factors, including the development of anoxic layers on the sediment–water interface and Si‐induced desorption from Fe, Al and Mn oxides. Internal P loading during the stratified period was thus estimated at about 4–9 g/m², suggesting that rapid changes in the lake's trophic status are at present unlikely. Certain aspects of this work (including interpretation of interrelationships between ecosystem components, estimation of the decomposition constant, analysis of factors controlling nutrient accumulation in the hypolimnion, and a low‐cost method to estimate internal P release) may be useful for studies of other aquatic systems and have, therefore, general limnological applicability. Copyright © 2001 John Wiley & Sons, Ltd.  相似文献   

Dynamics of phosphorus compounds in a lowland river system: Importance of retention and non-point sources     

Lars M. Svendsen  Brian Kronvang  Peter Kristensen  Peter Grsbl 《水文研究》1995,9(2):119-142

Intensive measurements of the fluxes of phosphorus (P) and of P retention were carried out in a Danish lowland watershed (Gjern Å) during two hydrological years (June 1987 to May 1989). Seasonal and short-term variations of P concentrations were measured by intensive automatic sampling covering P fluxes from the entire Gjern Å watershed and two subcatchments: the Gelbæk and Lake Søbygård. Moreover, infrequent sampling was performed in all major tributaries of the river system. Transport of P compounds (dissolved and particulate P) exposed a seasonal pattern which was highly affected by flow conditions, instream processes, as well as point and non-point sources. Stormflow P transport during the two study years (1987-8 and 1988-9) constituted 56 and 61% in the Gelbæk, respectively, compared with 25 and 23% in the Gjern Å, respectively. Particulate P transport in the Gelbæk constituted 56 and 75% of annual total P transport during the two years compared with 77 and 75% in the Gjern Å. The magnitude of monthly baseflow and stormflow total P loads was significantly correlated with the mean monthly discharge during baseflow and stormflow in the Gelbæk, whereas only stormflow loads were correlated to discharge in the Gjern Å. In situ measurements of retention showed that the maximum amount of P stored in the Gelbæk during summer (June to August) was 22gPm^?2 (1988) compared with 27gPm^?2 (1987) in the Gjern Å. Lake Søbygård was a P source during summer but a P sink during winter and on an annual basis the net P released was 810 and 1420 kg, which corresponded to 7 and 20% of the annual P export from the watershed, respectively. Retention constituted about 30% of gross P transport in the Gelbæk during summer compared with 20% in the Gjern Å. Resuspension of retained P during stormflows in September 1987 constituted 94% of the stormflow P transport and 54% of the total P transport. Monthly total P and dissolved reactive P (DRP) mass balances for the main channel of the Gjern Å revealed a significant DRP retention over 17 months (p < 0.05) caused by P adsorption on sediments and biological uptake. On an annual basis the main channel was a sink of DRP (1220 and 1660 kg P) but a source of total P (3440 and 1000 kg P). implying that the channel is an important source of particulate P. Bank erosion proved to be a significant P source in the main channel of Gjern Å, whereas P delivery from soil erosion was possibly of minor importance. The annual non-point P export from two intensively sampled catchments was significantly higher (0.89 and 0.45 kg Pha^?1 yr^?1) than from the five extensively sampled subbasins (0.43 and 0.17 kg Pha^?1 yr^?1). No significant relationship could be established between non-point P export and the proportion of arable land and soil type. Only for the wet year of 1987-8 was a significant relationship established between non-point P export and the P load from scattered dwellings outside sewage areas in five subbasins.  相似文献