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| Content Provider | Springer Nature Link |
|---|---|
| Author | Bustos Medina, Diego A. Berg, Gerard A. Breukelen, Boris M. Juhasz Holterman, Maria Stuyfzand, Pieter J. |
| Copyright Year | 2013 |
| Abstract | Clogging of water wells by iron-hydroxide incrustations due to mixing of anoxic and oxic groundwater is a common well-ageing problem. The relation between well operation (on and off), the spatial and temporal variations in hydrochemistry outside and inside a supply well, and the distribution of clogging iron-hydroxides were studied in an artificial recharge well field in the Netherlands. Camera inspection, high-resolution multi-level water sampling outside the well and detailed in-well pH/EC/O$_{2}$ profiles revealed remarkable patterns. During pumping, the top of the upper well screen abstracted oxic filtrate, although the larger part of the in-well water column was anoxic. The column rapidly turned oxic after shutdown due to a downward short-circuiting of oxic water via the well. Within 15 d it became anoxic due to the slow advance of anoxic lake filtrate created by local changes in flow direction as the neighboring wells continued to pump. Severe clogging occurred where the oxic filtrate entered the well, while half-clogging of the upper well screen occurred due to less inflow of oxic filtrate on the lake side. Transport of iron flocs and bacterial slimes after shutdown seemed to clog the lower part of the well screen. Frequent on/off switching should be avoided in iron-clogged wells.L’occlusion de puits par des incrustations d’hydroxyde de fer générées par le mélange d’eau anoxique et d’eau riche en oxygène est un problème courant de vieillissement des puits. La relation entre le fonctionnement du puits (par intermittence), les variations spatiales et temporelles de l’hydrogéochimie à l’extérieur et à l’intérieur du puits d’alimentation et la répartition des hydroxydes de fer qui l’obstruent ont été étudiées dans un champ de puits de recharge artificielle aux Pays Bas. L’inspection par caméra, l’échantillonnage de l’eau à des niveaux précis multiples à l’extérieur du puits et des profils détaillés de pH/EC/O$_{2}$ à l’intérieur ont révélé des configurations remarquables. Pendant le pompage, le haut de la crépine supérieure du puits extrayait une eau d’infiltration oxygénée, alors que la plus grande partie de la colonne d‘eau à l’intérieur du puits était anoxique. La colonne liquide s’est rapidement oxygénée après l’arrêt du pompage en raison du reflux direct de haut en bas dans le puits de l’eau riche en oxygène. En 15 jours, elle est devenue anoxique à la suite de la lente avancée d’une infiltration pauvre en oxygène venue d’un lac, causée par des changements locaux de la direction d’écoulement à un moment où les puits voisins continuaient à pomper. Une occlusion sévère est survenue au point où l’infiltration oxygénée a pénétré dans le puits, tandis qu’une demi-occlusion de la crépine supérieure du puits se produisait à la suite d’une intrusion moindre de l’infiltration oxygénée du côté du lac. La migration des flocs ferrugineux et des boues bactériennes après l’arrêt semblait obstruer la partie basse de la crépine du puits. Des démarrages et arrêts fréquents devraient être évités dans les puits obstrués par le fer.La obstrucción de pozos de agua por incrustaciones de hidróxido de hierro debido a la mezcla de agua subterránea anóxica y óxica es un problema común del envejecimiento de los pozos. Se estudiaron las relaciones entre la operación (encendido y apagado), las variaciones espaciales y temporales en la hidroquímica dentro y fuera de un pozo de abastecimiento, y la distribución de la obstrucción del hidróxido de hierro en un campo de pozos de recarga artificial en Holanda. Las inspecciones por cámaras, muestreos de agua multinivel de alta resolución fuera del pozo y perfiles detallados dentro del pozo de pH/EC/O$_{2}$ revelaron los patrones destacables. Durante en bombeo, el tope de la parte superior del filtro del pozo extrajo filtrados óxicos, aunque la mayor parte de la columna de agua dentro del pozo era anóxica. La columna rápidamente se convirtió en óxica después de una parada debido a un breve circuito descendente de agua óxica a través del pozo. Dentro de los 15 días se convirtió en anóxica debido al lento avance de la filtración del lago anóxico creado por cambios locales en la dirección de flujo a medida que los pozos vecinos continuaban el bombeo. Las obstrucciones severas ocurrieron cuando el filtrado óxico entró en el pozo, mientras que obstrucciones medias del filtro superior de la parte superior del pozo ocurrieron debido a un menor influjo del filtrado óxico hacia la margen del lago. El transporte de flóculos de hierro y el fango bacteriano después de la parada parecieron obstruir la parte inferior del filtro del pozo. Se debe evitar un frecuente cambio de encendido y apagado en los pozos obstruidos por el hierro.含氧和缺氧地下水的混合造成井中铁-氢氧化物水垢水堵塞是一种常见的水井老化问题。本文对荷兰一个人工补给井场的井(关机、开启)运行之间的关系、供水井内外空间和时间上的变化、以及铁-氢氧化物堵塞的分布进行了研究。摄像机检查、高分辨率多层次的井外取样和详细的井内pH、EC、O$_{2}$剖面揭示了值得注意的模式。在抽水期间,尽管井内水柱大部分缺氧,但水井滤水管上部的顶部抽取了含氧滤液。停止抽水后,由于通过水井的含氧水向下的短路循环,水柱迅速变为含氧。随着附近水井继续抽水,水流方向的局部变化造成的缺氧湖泊滤液缓慢移动,15天之内,水变为缺氧。在含氧滤液进入水井的地方,出现了严重的堵塞,而水井滤水管上部出现半堵塞,这是因为湖泊边的含氧滤液的流入较少。停车抽水后铁屑和细菌黏质的运移似乎堵塞了水滤水管的下部。在铁堵塞的水井中应避免频繁的开/停抽水。A colmatação de furos de água por incrustações de hidróxido de ferro, devido à mistura de água subterrânea anóxica e óxica, é um problema de envelhecimento de furos bastante comum. Num campo de recarga artificial de furos na Holanda, foram estudadas a relação entre a exploração do furo (ligar e desligar), as variações espaciais e temporais na hidroquímica no interior de um furo de abastecimento e nas suas vizinhanças e a distribuição da colmatação por hidróxidos de ferro. A inspeção através de câmara, a amostragem de água multinível de alta resolução na vizinhança do furo e perfis detalhados de pH/EC/O$_{2}$ no interior do furo revelaram padrões notáveis. Durante o bombeamento, o topo do ralo superior produziu filtrado óxico, apesar da maior parte da coluna de água no furo ser anóxica. Após a paragem, a coluna de água tornou-se rapidamente óxica, devido a um pequeno circuito descendente de água óxica através do furo. Ao fim de 15 dias, o furo tornou-se anóxico, devido ao avanço lento do filtrado anóxico de um lago, motivado por alterações locais na direção do fluxo pelo fato dos furos vizinhos continuarem em exploração. Ocorreu colmatação grave quando o filtrado óxico entrou no furo, enquanto no ralo superior do furo ocorreu colmatação parcial, devido à menor afluência de filtrado óxico do lado do lago. Após a paragem do furo, o transporte de flocos de ferro e limos baterianos parecia obstruir a parte inferior do ralo. Em furos colmatados por ferro devem ser evitadas as paragens e arranques frequentes. |
| Starting Page | 1393 |
| Ending Page | 1412 |
| Page Count | 20 |
| File Format | |
| ISSN | 14312174 |
| Journal | Hydrogeology Journal |
| Volume Number | 21 |
| Issue Number | 7 |
| e-ISSN | 14350157 |
| Language | Portuguese |
| Publisher | Springer Berlin Heidelberg |
| Publisher Date | 2013-07-18 |
| Publisher Institution | International Association of Hydrogeologists |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Water supply The Netherlands Hydrochemistry Iron-hydroxides Well clogging Hydrogeology Hydrology/Water Resources Geology Waste Water Technology Water Pollution Control Water Management Aquatic Pollution |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth and Planetary Sciences Water Science and Technology |
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