خيارات البحث
النتائج 1301 - 1310 من 1,363
A parsimonious distributed model for simulating transient water flow in a high-relief karst aquifer | Un modèle spatialisé parcimonieux de simulation des écoulements transitoires dans un aquifère karstique de montagne Un modelo distribuido parsimonioso para similar flujo transitorio en un acuífero kárstico de relieve alto 模拟高峻地形岩溶含水层瞬时水流的一个简约分布式模型 Um modelo de distribuição parcimoniosa para simular fluxo transitório de água em um aquífero cárstico de alto relevo النص الكامل
2018
Pardo-Igúzquiza, Eulogio | Dowd, P. A. | Pulido Bosch, Antonio | Luque-Espinar, Juan A. | Heredia, Javier | Durán-Valsero, Juan J.
A parsimonious distributed model for simulating transient water flow in a high-relief karst aquifer | Un modèle spatialisé parcimonieux de simulation des écoulements transitoires dans un aquifère karstique de montagne Un modelo distribuido parsimonioso para similar flujo transitorio en un acuífero kárstico de relieve alto 模拟高峻地形岩溶含水层瞬时水流的一个简约分布式模型 Um modelo de distribuição parcimoniosa para simular fluxo transitório de água em um aquífero cárstico de alto relevo النص الكامل
2018
Pardo-Igúzquiza, Eulogio | Dowd, P. A. | Pulido Bosch, Antonio | Luque-Espinar, Juan A. | Heredia, Javier | Durán-Valsero, Juan J.
A mathematical model of a highly heterogeneous functioning karst aquifer is described. The aquifer is in a high-relief karst massif and, as is common for such locations, data are scarce and there are no borehole, piezometer or pumping-test data. The scarcity of data in this case required a parsimonious approach to ensure that the level of complexity of the model was commensurate with the amount, type and quality of the available data. Parsimony also requires the model to include the minimum essential components that account adequately for the data, which in this and similar cases are the functional dualities of the karst system: duality in recharge, flow and discharge. The model is three-dimensional (3D) in the sense that the aquifer is discretized into 3D voxels, although the flow is one-dimensional (1D) and vertical in the vadose zone, and horizontal and two-dimensional (2D) in the saturated zone. The parsimonious model was designed by coupling a 1D unsaturated gravity-driven flow along the vertical (along each column of voxels that discretize the aquifer) and a 2D unconfined Darcy flow in the saturated zone. In the context of this type of aquifer, preferential recharge through the network of karst conduits implies a rapid rise in the water table, the location and extension of which are model parameters. The karst springs are simulated by drains. The methodology, which is completely general, is illustrated by application to the karst aquifer in the Sierra de las Nieves mountains in southern Spain.
اظهر المزيد [+] اقل [-]A parsimonious distributed model for simulating transient water flow in a high-relief karst aquifer النص الكامل
2018
Pardo-Igúzquiza, E. | Dowd, P. | Bosch, A. | Luque-Espinar, J. | Heredia, J. | Durán-Valsero, J.
A mathematical model of a highly heterogeneous functioning karst aquifer is described. The aquifer is in a high-relief karst massif and, as is common for such locations, data are scarce and there are no borehole, piezometer or pumping-test data. The scarcity of data in this case required a parsimonious approach to ensure that the level of complexity of the model was commensurate with the amount, type and quality of the available data. Parsimony also requires the model to include the minimum essential components that account adequately for the data, which in this and similar cases are the functional dualities of the karst system: duality in recharge, flow and discharge. The model is three-dimensional (3D) in the sense that the aquifer is discretized into 3D voxels, although the flow is one-dimensional (1D) and vertical in the vadose zone, and horizontal and two-dimensional (2D) in the saturated zone. The parsimonious model was designed by coupling a 1D unsaturated gravity-driven flow along the vertical (along each column of voxels that discretize the aquifer) and a 2D unconfined Darcy flow in the saturated zone. In the context of this type of aquifer, preferential recharge through the network of karst conduits implies a rapid rise in the water table, the location and extension of which are model parameters. The karst springs are simulated by drains. The methodology, which is completely general, is illustrated by application to the karst aquifer in the Sierra de las Nieves mountains in southern Spain. | Eulogio Pardo-Igúzquiza, Peter Dowd, Antonio Pulido Bosch, Juan A. Luque-Espinar, Javier Heredia, Juan J. Durán-Valsero
اظهر المزيد [+] اقل [-]Simplification of the Gardner model: effects on maximum upward flux in the presence of a shallow water table | Simplification du modèle de Gardner: effets sur le flux ascendant en présence d’une nappe phréatique peu profonde Simplificación del modelo de Gardner: efectos sobre el flujo ascendente máximo en presencia de un nivel freático superficial Gardner模型简化对地下水浅埋条件极限蒸发强度的影响 Simplificação do modelo de Gardner: efeitos do fluxo vertical máximo pela presença de níveis de água rasos النص الكامل
2018
Xing, Xuguang | Ma, Xiaoyi
The maximum upward flux (Eₘₐₓ) is a control condition for the development of groundwater evaporation models, which can be predicted through the Gardner model. A high-precision Eₘₐₓ prediction helps to improve irrigation practice. When using the Gardner model, it has widely been accepted to ignore parameter b (a soil-water constant) for model simplification. However, this may affect the prediction accuracy; therefore, how parameter b affects Eₘₐₓ requires detailed investigation. An indoor one-dimensional soil-column evaporation experiment was conducted to observe Eₘₐₓ in the presence of a water table of depth 50 cm. The study consisted of 13 treatments based on four solutes and three concentrations in groundwater: KCl, NaCl, CaCl₂, and MgCl₂, with concentrations of 5, 30, and 100 g/L (salty groundwater); distilled water was used as a control treatment. Results indicated that for the experimental homogeneous loam, the average Eₘₐₓ for the treatments supplied by salty groundwater was larger than that supplied by distilled water. Furthermore, during the prediction of the Gardner-model-based Eₘₐₓ, ignoring b and including b always led to an overestimate and underestimate, respectively, compared to the observed Eₘₐₓ. However, the maximum upward flux calculated including b (i.e. Ebₘₐₓ) had higher accuracy than that ignoring b for Eₘₐₓ prediction. Moreover, the impact of ignoring b on Eₘₐₓ gradually weakened with increasing b value. This research helps to reveal the groundwater evaporation mechanism.
اظهر المزيد [+] اقل [-]Prediction of water inflow to mechanized tunnels during tunnel-boring-machine advance using numerical simulation | Prévision des débits de venues d’eau dans les tunnels mécanisés, au cours du creusement au tunnelier, à l’aide de simulations numériques Predicción mediante simulación numérica del flujo de agua a túneles mecanizados durante el avance de la máquina perforadora de túneles 利用数值模拟预测隧道掘进机开挖期间隧道的涌水 پیشبینی آب ورودی به تونلهای مکانیزه به ازای پیشروی حفاری دستگاه TBM به روش شبیهسازی عددی النص الكامل
2018
Golian, Mohsen | Teshnizi, Ebrahim Sharifi | Nakhaei, Mohammad
An accurate estimate of the groundwater inflow to a tunnel is one of the most challenging but essential tasks in tunnel design and construction. Most of the numerical or analytical solutions that have been developed ignore tunnel seepage conditions, material properties and hydraulic-head changes along the tunnel route during the excavation process, leading to inaccurate prediction of inflow rates. A method is introduced that uses MODFLOW code of GMS software to predict inflow rate as the tunnel boring machine (TBM) gradually advances. In this method, the tunnel boundary condition is conceptualized and defined using Drain package, which is simulated by dividing the drilling process into a series of successive intervals based on the tunnel excavation rates. In addition, the drain elevations are specified as the respective tunnel elevations, and the conductance parameters are assigned to intervals, depending on the TBM type and the tunnel seepage condition. The Qomroud water conveyance tunnel, located in Lorestan province of Iran, is 36 km in length. Since the Qomroud tunnel involved groundwater inrush during excavating, it is considered as a good case study to evaluate the presented method. The groundwater inflow to this tunnel during the TBM advance is simulated using the proposed method and the predicted rates are compared with observed rates. The results show that the presented method can satisfactorily predict the inflow rates as the TBM advances.
اظهر المزيد [+] اقل [-]Using stable isotopes (δD, δ18O, δ34S and 87Sr/86Sr) to identify sources of water in abandoned mines in the Fengfeng coal mining district, northern China | Utilisation des isotopes stables (δD, δ18O, δ34S and 87Sr/86Sr) pour identifier l’origine de l’eau dans des mines abandonnées dans le district des mines de charbon de Fengfeng dans le Nord de la Chine Uso de isótopos estables (δD, δ18O, δ34S and 87Sr/86Sr) Para identificar las Fuentes de agua en minas abandonadas en el distrito minero de carbón de Fengfeng, norte de China 利用稳定同位素(δD,δ18O,δ34S和87Sr/86Sr)识别华北峰峰矿区废弃矿井充水水源 Uso de isótopos estáveis (δD, δ18O, δ34S e 87Sr/86Sr) Para identificar fontes de água em minas abandonadas no distrito de mineração de carvão de Fengfeng, norte da China النص الكامل
2018
Qu, Shen | Wang, Guangcai | Shi, Zheming | Xu, Qingyu | Guo, Yuying | Ma, Luan | Sheng, Yizhi
With depleted coal resources or deteriorating mining geological conditions, some coal mines have been abandoned in the Fengfeng mining district, China. Water that accumulates in an abandoned underground mine (goaf water) may be a hazard to neighboring mines and impact the groundwater environment. Groundwater samples at three abandoned mines (Yi, Er and Quantou mines) in the Fengfeng mining district and the underlying Ordovician limestone aquifer were collected to characterize their chemical and isotopic compositions and identify the sources of the mine water. The water was HCO₃·SO₄-Ca·Mg type in Er mine and the auxiliary shaft of Yi mine, and HCO₃·SO₄-Na type in the main shaft of Quantou mine. The isotopic compositions (δD and δ¹⁸O) of water in the three abandoned mines were close to that of Ordovician limestone groundwater. Faults in the abandoned mines were developmental, possibly facilitating inflows of groundwater from the underlying Ordovician limestone aquifers into the coal mines. Although the Sr²⁺ concentrations differed considerably, the ratios of Sr²⁺/Ca²⁺ and ⁸⁷Sr/⁸⁶Sr and the ³⁴S content of SO₄²⁻ were similar for all three mine waters and Ordovician limestone groundwater, indicating that a close hydraulic connection may exist. Geochemical and isotopic indicators suggest that (1) the mine waters may originate mainly from the Ordovician limestone groundwater inflows, and (2) the upward hydraulic gradient in the limestone aquifer may prevent its contamination by the overlying abandoned mine water. The results of this study could be useful for water resources management in this area and other similar mining areas.
اظهر المزيد [+] اقل [-]Modes, hydrodynamic processes and ecological impacts exerted by river–groundwater transformation in Junggar Basin, China | Modalités, processus hydrodynamiques et impacts écologiques exercés par les transformations sur les relations entre les eaux de surface et les eaux souterraines dans le bassin de Junggar, Chine Modos, procesos hidrodinámicos e impactos ecológicos ejercidos por la transformación río–agua subterránea en la Cuenca de Junggar, China 中国准格尔盆地河流–地下水转换模式、水动力过程以及引起的生态影响 Modos, processos hidrodinâmicos e impactos ecológicos exercidos pela transformação água subterrânea–rio na Bacia Junggar, China النص الكامل
2018
Wang, Wenke | Wang, Zhan | Hou, Rongzhe | Cunha, Luís Sá | Dang, Yan | Zhang, Zaiyong | Wang, Hao | Duan, Lei | Wang, Zhoufeng
The hydrodynamic processes and impacts exerted by river–groundwater transformation need to be studied at regional and catchment scale, especially with respect to diverse geology and lithology. This work adopted an integrated method to study four typical modes (characterized primarily by lithology, flow subsystems, and gaining/losing river status) and the associated hydrodynamic processes and ecological impacts in the southern part of Junggar Basin, China. River–groundwater transformation occurs one to four times along the basin route. For mode classification, such transformation occurs: once or twice, controlled by lithological factors (mode 1); twice, impacted by geomorphic features and lithological structures (mode 2); and three or four times, controlled by both geological and lithological structures (modes 3 and 4). Results also suggest: (1) there exist local and regional groundwater flow subsystems at ~400 m depth, which form a multistage nested groundwater flow system. The groundwater flow velocities are 0.1–1.0 and <0.1 m/day for each of two subsystems; (2) the primary groundwater hydro-chemical type takes on apparent horizontal and vertical zoning characteristics, and the TDS of the groundwater evidently increases along the direction of groundwater flow, driven by hydrodynamic processes; (3) the streams, wetland and terminal lakes are the end-points of the local and regional groundwater flow systems. This work indicates that not only are groundwater and river water derived from the same source, but also hydrodynamic and hydro-chemical processes and ecological effects, as a whole in arid areas, are controlled by stream–groundwater transformation.
اظهر المزيد [+] اقل [-]IET for the environmental monitoring of the intensive production of tilapia in cage in the Atlantic Forest region of South America | Índice de estado trófico e qualidade da água na produção de tilápias em tanques-rede em represa rural na região da Mata Atlântica na América do Sul النص الكامل
2018
Leonardo, A.F. | Baccarin, A.E. | Trombeta, T.D. | Machado, L.P. | Teramoto, E.T. | Bueno, G.W.
The production of tilapia (Oreochromis niloticus) in cages requires the constant monitoring of the physical and chemical water properties, since it is an activity considered potentially polluting for the aquatic environment and its monitoring is fundamental to avoid the water body eutrophication processes. The present study was conducted in a reservoir located in a fishfarm at Pariquera – Açu County (São Paulo state, Brazil) and evaluated the influence of the intensive Nile tilapia production in cages on the trophic state and in the water quality. For the trophic state determination, five classes were considered and stablished by the Trophic State Index (TSI). The trial was developed and divided in three phases: before (90 days), during (180 days) and after (90 days) the fish intensive production in the reservoir. Thirty net cages with volume of 4 m3 and stocking density of 150 fish per m3 were installed. According to the results, it was observed that the trophic state index (TSI) was increasing according to the production period, changing from an ultra-oligotrophic to a mesotrophic state, reaching a maximum value of 53.2 ± 0.4, and, after production period, remained oligotrophic. The water quality parameters did not present significant differences between the periods analysed (p>0.05). The implementation of the TSI represents a practical tool for environmental monitoring and risk analysis of fish production in the aquatic environment. | A produção de tilápias (Oreochromis niloticus) em tanques-rede exige o constante monitoramento das propriedades físico-químicas da água, pois é uma atividade considerada potencialmente poluidora do ambiente aquático e o monitoramento é fundamental para evitar processos de eutrofização do corpo hídrico. O presente estudo avaliou a influência da produção intensiva de tilápia do Nilo em tanques-rede sobre o grau de trofia e qualidade da água em uma represa localizada no Vale do Ribeira, região de Mata Atlântica no sudeste do Brasil. Na classificação do grau de trofia foram considerados cinco classes, que foram estabelecidas a partir do Índice do Estado Trófico (IET). O experimento foi conduzido em três períodos: antes (90 dias), durante (180 dias) e após (90 dias) à produção intensiva de peixes na represa. Instalaram-se 30 tanques-rede de 4 m3 com densidade de estocagem de 150 peixes por m3. A partir dos resultados experimentais, verificou-se que o IET foi crescente no período de produção passando de ultraoligotrófico à mesotrófico, alcançou valor máximo de 53,2 ± 0,4 e após a produção manteve-se oligotrófico. Os parâmetros de qualidade de água não apresentaram diferenças significativas entre os períodos analisados (p>0.05). A aplicação com base no IET representa uma ferramenta prática para o monitoramento ambiental e análise de riscos da produção de peixes no ambiente aquático.
اظهر المزيد [+] اقل [-]Comparison of specific-yield estimates for calculating evapotranspiration from diurnal groundwater-level fluctuations | Comparaison de valeurs estimées de porosité efficace pour calculer l’évapo-transpiration à partir de fluctuations piézométriques diurnes Comparación de estimaciones de rendimiento específico para calcular la evapotranspiración a partir de las fluctuaciones diurnas del nivel del agua subterránea 对单位出水量估算值进行对比,进而根据白天地下水位波动计算蒸发蒸腾量 Comparação de estimativas de rendimento especifico para o cálculo da evapotranspiração a partir de flutuações diurnas do nível da água subterrânea النص الكامل
2018
Gribovszki, Zoltán
Methods that use diurnal groundwater-level fluctuations are commonly used for shallow water-table environments to estimate evapotranspiration (ET) and recharge. The key element needed to obtain reliable estimates is the specific yield (Sy), a soil-water storage parameter that depends on unsaturated soil-moisture and water-table fluxes, among others. Soil-moisture profile measurement down to the water table, along with water-table-depth measurements, can provide a good opportunity to calculate Sy values even on a sub-daily scale. These values were compared with Sy estimates derived by traditional techniques, and it was found that slug-test-based Sy values gave the most similar results in a sandy soil environment. Therefore, slug-test methods, which are relatively cheap and require little time, were most suited to estimate Sy using diurnal fluctuations. The reason for this is that the timeframe of the slug-test measurement is very similar to the dynamic of the diurnal signal. The dynamic characteristic of Sy was also analyzed on a sub-daily scale (depending mostly on the speed of drainage from the soil profile) and a remarkable difference was found in Sy with respect to the rate of change of the water table. When comparing constant and sub-daily (dynamic) Sy values for ET estimation, the sub-daily Sy application yielded higher correlation, but only a slightly smaller deviation from the control ET method, compared with the usage of constant Sy.
اظهر المزيد [+] اقل [-]Dynamics of greenhouse gases in the river–groundwater interface in a gaining river stretch (Triffoy catchment, Belgium) | Dynamique des gaz à effet de serre à l’interface rivière–eau souterraine dans un tronçon drainant de la rivière (bassin versant du Triffoy, Belgique) Dinámica de los gases de efecto invernadero en la interfaz río–agua subterránea en un tramo de río ganador (Cuenca Triffoy, Bélgica) (比利时Triffoy流域)一个袭夺河段中河水–地下水界面温室气体动力学 Dinâmica de gases de efeito estufa na interface rio - água subterrânea em um trecho de ganho fluvial (bacia de Triffoy, Bélgica) النص الكامل
2018
Jurado, Anna | Borges, Alberto V. | Pujades, Estanislao | Briers, Pierre | Nikolenko, Olha | Dassargues, Alain | Brouyère, Serge
Dynamics of greenhouse gases in the river–groundwater interface in a gaining river stretch (Triffoy catchment, Belgium) | Dynamique des gaz à effet de serre à l’interface rivière–eau souterraine dans un tronçon drainant de la rivière (bassin versant du Triffoy, Belgique) Dinámica de los gases de efecto invernadero en la interfaz río–agua subterránea en un tramo de río ganador (Cuenca Triffoy, Bélgica) (比利时Triffoy流域)一个袭夺河段中河水–地下水界面温室气体动力学 Dinâmica de gases de efeito estufa na interface rio - água subterrânea em um trecho de ganho fluvial (bacia de Triffoy, Bélgica) النص الكامل
2018
Jurado, Anna | Borges, Alberto V. | Pujades, Estanislao | Briers, Pierre | Nikolenko, Olha | Dassargues, Alain | Brouyère, Serge
This study investigates the occurrence of greenhouse gases (GHGs) and the role of groundwater as an indirect pathway of GHG emissions into surface waters in a gaining stretch of the Triffoy River agricultural catchment (Belgium). To this end, nitrous oxide (N₂O), methane (CH₄) and carbon dioxide (CO₂) concentrations, the stable isotopes of nitrate, and major ions were monitored in river and groundwater over 8 months. Results indicated that groundwater was strongly oversaturated in N₂O and CO₂ with respect to atmospheric equilibrium (50.1 vs. 0.55 μg L⁻¹ for N₂O and 14,569 vs. 400 ppm for CO₂), but only marginally for CH₄ (0.45 vs. 0.056 μg L⁻¹), suggesting that groundwater can be a source of these GHGs to the atmosphere. Nitrification seemed to be the main process for the accumulation of N₂O in groundwater. Oxic conditions prevailing in the aquifer were not prone for the accumulation of CH₄. In fact, the emissions of CH₄ from the river were one to two orders of magnitude higher than the inputs from groundwater, meaning that CH₄ emissions from the river were due to CH₄ in-situ production in riverbed or riparian zone sediments. For CO₂ and N₂O, average emissions from groundwater were 1.5 × 10⁵ kg CO₂ ha⁻¹ year⁻¹ and 207 kg N₂O ha⁻¹ year⁻¹, respectively. Groundwater is probably an important source of N₂O and CO₂ in gaining streams but when the measures are scaled at catchment scale, these fluxes are probably relatively modest. Nevertheless, their quantification would better constrain nitrogen and carbon budgets in natural systems.
اظهر المزيد [+] اقل [-]Dynamics of greenhouse gases in the river–groundwater interface in a gaining river stretch (Triffoy catchment, Belgium) النص الكامل
2018
Jurado, Anna | Borges, Alberto | Pujades, Estanislao | Briers, Pierre | Nikolenko, Olha | Dassargues, Alain | Brouyère, Serge | UEE - Urban and Environmental Engineering - ULiège | FOCUS - Freshwater and OCeanic science Unit of reSearch - ULiège
peer reviewed | This study investigates the occurrence of greenhouse gases (GHGs) and the role of groundwater as an indirect pathway of GHG emissions into surface waters in a gaining stretch of the Triffoy River agricultural catchment (Belgium). To this end, nitrous oxide (N2O), methane (CH4) and carbon dioxide (CO2) concentrations, the stable isotopes of nitrate, and major ions were monitored in river and groundwater over 8 months. Results indicated that groundwater was strongly oversaturated in N2O and CO2 with respect to atmospheric equilibrium (50.1 vs. 0.55 μg L−1 for N2O and 14,569 vs. 400 ppm for CO2), but only marginally for CH4 (0.45 vs. 0.056 μg L−1), suggesting that groundwater can be a source of these GHGs to the atmosphere. Nitrification seemed to be the main process for the accumulation of N2O in groundwater. Oxic conditions prevailing in the aquifer were not prone for the accumulation of CH4. In fact, the emissions of CH4 from the river were one to two orders of magnitude higher than the inputs from groundwater, meaning that CH4 emissions from the river were due to CH4 in-situ production in riverbed or riparian zone sediments. For CO2 and N2O, average emissions from groundwater were 1.5 × 105 kg CO2 ha−1 year−1 and 207 kg N2O ha−1 year−1, respectively. Groundwater is probably an important source of N2O and CO2 in gaining streams but when the measures are scaled at catchment scale, these fluxes are probably relatively modest. Nevertheless, their quantification would better constrain nitrogen and carbon budgets in natural systems.
اظهر المزيد [+] اقل [-]COMPARACIÓN DEL EFECTO DE DOS TRATAMIENTOS ENZIMÁTICOS CON ACTIVIDAD COLAGENASA Y UNA CENTRIFUGACIÓN COMPLEMENTARIA EN LAS CARACTERÍSTICAS FISICOQUÍMICAS DEL AGUA DE COLA GENERADA POR LA INDUSTRIA SARDINERA | COMPARISON OF THE EFFECT OF TWO ENZYMATIC TREATMENTS WITH COLLAGENASE ACTIVITY AND A COMPLEMENTARY CENTRIFUGATION ON THE PHYSICOCHEMICAL CHARACTERISTICS OF FISHMEAL INDUSTRY STICKWATER النص الكامل
2018
Ramón Pacheco Aguilar | Ana María Calderón de la Barca | FRANCISCO JAVIER CASTILLO YAÑEZ | ENRIQUE MARQUEZ RIOS | Fernando Luis García Carreño | SANTIAGO VALDEZ HURTADO
"Se evaluó el efecto de las enzimas de vísceras de sardi¬na Monterey en el tratamiento del agua de cola producida por sardinas crinuda y Monterey y, se compararon con enzimas de un extracto comercial. Además, se aplicó una centrifugación complementaria al ensayo. La enzima comercial tuvo mayor actividad proteasa que la enzima de víscera de sardina (0.65 U/mg vs. 0.35 U/mg) y que la actividad colagenasa (0.022 Hyp/mg/min vs. 0.0102 Hyp/mg/min). Se observaron grados de hidrolisis mayores sobre agua de cola de sardina crinuda (16.1 %), y no se registraron diferencias significativas (P≥0.05) en el agua de cola de sardina Monterey por el uso de las en¬zimas de vísceras de sardina Monterey y enzimas comercial. Se obtuvo mayor hidrolisis al aplicar la enzima de víscera de sardina Monterey sobre el agua de cola centrifugada (57.1 % vs. 17.4 %) sin importar la especie de sardina utilizada. La enzima comercial disminuyó la viscosidad sobre el agua de cola, mientras que la enzima de víscera de sardina Monterey lo hizo sobre el agua de cola centrifugada. La electroforesis mostró una disminución de la fracción PM>220 kDa en el agua de cola. Lo anterior, indicó que la enzima comercial tuvo una mayor actividad sobre agua de cola, mientras que la enzima de víscera de sardina Monterey lo tuvo en agua de cola centrifugada, sin importar el tipo de sardina utilizada para la elaboración del agua de cola." | "We evaluated the effect of Monterey sardines viscera enzyme on stickwater treatment produced by crinude and Monterey sardines and compared with commercial enzyme. In addition, we applied a complementary centrifugation to add in test. Commercial enzyme has greater protease activity than Monterey sardines viscera (0.65 U/mg vs. 0.35 U/mg) and collagenase activity (0.022 Hyp/mg/min vs. 0.0102 Hyp/mg/ min). Higher degree of hydrolysis on stickwater from crinude sardine (16.1 %), and no significant differences (P≥0.05) on stickwater from Monterey sardine between commercial en¬zyme and Monterey sardine viscera were observed. Degree of hydrolysis increased to application Monterey sardines vis¬cera on centrifuged stickwater (57.1 % vs. 17.4 %) regardless of which sardine specie it came from. Commercial enzyme reduced viscosity on stickwater while Monterey sardines viscera did it on centrifuged stickwater. The electrophoresis showed reduction on MW>220 kDa fraction in stickwater. The above, showed that commercial enzyme have a better activity on stickwater while Monterey sardines viscera did it better on the centrifuged stickwater, regardless sardine specie which the stickwater came from."
اظهر المزيد [+] اقل [-]Evaluación del dimensionamiento de la laguna de oxidación, propuesta para el mejoramiento del sistema de tratamiento de agua residual del puesto de mando adelantado (PMAD) los Mangos | Evaluation of the dimensions of the oxidation pond, proposal for the improvement of the wastewater treatment system of the puesto de mando adelantado los Mangos (PMAD) النص الكامل
2018
Luna Mendoza, Angie Lorena | Agualimpia Dualiby, Yolima del Carmen | Pulido Tovar, Erika Tatiana
El Comando de Ingenieros (COING) del Ejército Nacional de Colombia, adelanta estudios para realizar una adecuación de la planta de tratamiento de agua residual del Puesto de Mando Adelantado (PMAD) Los Mangos, ubicado en el Fuerte Militar de Tolemaida. La sugerencia del COING se centra en la construcción de una laguna de oxidación que pueda eliminar de forma natural los patógenos y materia orgánica provenientes de las actividades domésticas del batallón. Actualmente el Batallón de Apoyo de Servicios para la Educación Militar (BASEM) es el encargado de llevar un seguimiento a las actividades realizadas en el PMAD. Los Mangos, no obstante, dicha unidad militar no cuenta con soportes técnicos de las dimensiones de la laguna de oxidación propuesta por el COING, de manera que, se realiza una evaluación con base a criterios establecidos por el Centro Panamericano de Ingeniería Sanitaria y Ciencias del Ambiente (CEPIS), para garantizar viabilidad, control y funcionalidad de la misma. Según los parámetros fisicoquímicos que favorecen el proceso y las características propias del diseño, se determina que es una laguna facultativa, por lo tanto, su periodo de retención debe estar dentro del rango de 5 a 30 días, sin embargo, al evaluar éste parámetro fundamental para la eficiencia de la laguna, se estimó un tiempo de 2.71 días. Para cumplir con éste criterio, se recomienda que la profundidad no sea de 1.5 m sino de 2.5 m, teniendo en cuenta que el tiempo de retención hidráulico depende principalmente de la forma, tamaño y del flujo disperso en la laguna. De ésta manera se obtendrán remociones eficientes tanto de coliformes fecales como de DBO. Para obtener resultados favorables en el tratamiento de las aguas residuales, además de contar con un diseño óptimo, es indispensable realizar mantenimiento periódico a la laguna de oxidación, y así evitar problemas como eutrofización, estancamientos, rupturas de membrana y vectores. | The COING [Comando de Ingenieros del Ejército Nacional de Colombia] advance in researches to adecuate the residual water treatment plant of the PMAD [Puesto de mando adelantado] Los Mangos located in the military base (Tolemaida-Colombia). The COING suggestion is focused in the construction of an oxidation pond that can eliminate in natural form pathogens and organic material originated from the domestic activities of the military base. The BASEM [Batallón de Apoyo de Servicios para la Educación Militar] is the responsible now to follow the activities realized in the PMAD los Mangos, nevertheless, this military unit does not have enough technical information about the oxidation pond dimensions proposed by the COING; that is why an evaluation is realized according with the criteria established by the CEPIS [Centro Panamericano de Ingeniería Sanitaria y Ciencias del Ambiente], to guarantee viability, control and functionality of the oxidation pond. According with the physically and chemical parameters who assist the process and the characteristics of the design, was determined it is a facultative pond; it needs an hydraulic retention time standard into the range of 5 to 30 days however at the moment of the evaluation the results showed 2.71 days. To achieve with this criteria it is recommended to change the depth from 1.5 to 2.5 meters, having in mind that the hydraulic retention time depends on the form, size and liquid dispersed into the pond. Working with this changes will be obtained efficient removal processes in thermotolerant (fecal) coliforms and Biological Oxygen Demand (BOD). To obtain better results in the residual water treatment it is necessary to have an optimal design and work periodically in the oxidation pond maintenance, to avoid problems like water eutrophication, blockages, membrane structure rupture and vectors. | Ejército Nacional de Colombia
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