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Grundakvo estas akvokvanto, kiu sub la ter … Grundakvo estas akvokvanto, kiu sub la tersurfaco formas akvokorpojn en la kavaĵoj (poroj). Ĝi situas super la unua akvoferma tavolo kaj tie plenigas la spacojn inter la grunderoj. La supra nivelo de la grundakvo estas la tersurfaco. La nivelo de la grundakvo en la grundo ŝanĝiĝas depende de la precipitaĵo, temperaturo, aerpremo, laŭ sezono. La normala jara ŝanĝiĝo de grundakvo estas 1-2 metroj. La grundakva nivelo pli-malpli sekvas paralele la geografian surfacon. Ĝi nutras sin el la precipitaĵa akvo kaj malrapide moviĝas al direkto de la deklivo. En la stagnanta grundakvo povas akumuliĝis damagaĵ saloj, tie lla altiĝo de la grundakvo povas kaŭzi , malproduktemiĝon de la grundo. La altiĝo de la grundakvo povas kaŭzi eĉ surfacajn akvokolektaĵojn, tiam la kapilara zono rekte kontaktas la aeron. Ĉar la alta-malalta grundakvo ne ĉiam konvenas por la plantoj, tiel oni povas reguligi ĝin en la agrikulturo per forkonduko de grundakvo aŭ alkonduko de akvo (ŝveligo de akvo en kanaloj).duko de akvo (ŝveligo de akvo en kanaloj).
, 지하수(地下水, 문화어: 땅속물)는 지표면 밑을 흐르는 물을 이르는 말이다. … 지하수(地下水, 문화어: 땅속물)는 지표면 밑을 흐르는 물을 이르는 말이다. 지구의 외부는 암석으로 이루어진 지각으로 덮여있고, 식물이 자라는 지표면 바로 밑에는 암석을 관통하여 물이 흐르고 있다. 대부분의 지하수는 흙 속으로 스며든 비와 눈이 녹은 물이 모여서 형성된다. 물은 암석에 도달하면 암석 사이의 열려 있는 틈을 통해 흐른다. 지하수가 흐르는 속도는 지하의 환경에 따라 일정하지 않아서 하루평균 1.5m 정도로 흐르는 곳도 있지만, 어떤 곳의 지하수는 연평균 약 1.5m의 속도로 아주 천천히 흐르기도 한다.어떤 곳의 지하수는 연평균 약 1.5m의 속도로 아주 천천히 흐르기도 한다.
, L'aigua subterrània representa una fracció … L'aigua subterrània representa una fracció important de la massa de aigua present en els continents, sota la superfície de la Terra, tant en el sòl com en el subsòl ja que, convencionalment, el terme inclou cert espessor com s'assenyala en l'article respectiu, en ser un concepte tridimensional. Evidentment, si solament fos bidimensional no podríem parlar d'aigua subterrània. El volum de l'aigua subterrània és molt més important que la massa d'aigua retinguda en llacs o circulant, i encara que menor al dels majors glacials, les masses més extenses poden aconseguir un milió o més de quilòmetres quadrats (com l'Aqüífer Guaraní). L'aigua del subsòl és un recurs important i d'aquest es proveeix a una tercera part de la població mundial, però de difícil gestió, per la seva sensibilitat a la contaminació i a la sobreexplotació. L'aigua subterrània és part de la precipitació que es filtra a través del sòl fins a arribar al material rocós que està saturat d'aigua. L'aigua subterrània es mou lentament cap als nivells baixos, generalment en angles inclinats (a causa de la gravetat) i finalment arriben als rierols, els llacs i els oceans. És una creença comuna que l'aigua subterrània plena cavitats i circula per galeries. No obstant això, no sempre és així, doncs pot trobar-se ocupant els (porus i esquerdes) del sòl, del substrat rocós o del sediment sense consolidar, els quals la contenen com una . L'única excepció significativa l'ofereixen les roques solubles, com les calcàrias i els guixos, susceptibles de sofrir el procés anomenat karstificació, en el qual l'aigua excava avencs, cavernes i altres vies de circulació, el model que més s'ajusta a la creença popular. Les masses d'aigua subterrània són un volum clarament diferenciat d'aigües subterrànies en un aqüífer o aqüífers. Un aqüífer és aquella massa de roques permeables que permet la circulació i l'acumulació de l'aigua subterrània en els seus porus o esquerdes. Les roques magatzem poden ser de materials molt variats com gravas i areniscas poroses poc cementades (antics sediments marins, de riu, platja, eòlics), llims, certs tipus d'argila, calcàries esquerdades, i fins i tot formacions volcàniques. El nivell superior de l'aigua subterrània es denomina taula d'aigua, que en el cas d'un aqüífer lliure correspon al nivell freàtic. És a dir, l'aqüífer és una o més capes subterrànies de roca o d'altres estrats geològics que tenen la suficient porositat i permeabilitat per permetre ja sigui un flux significatiu d'aigües subterrànies o l'extracció dequantitats significatives d'aigües subterrànies.tats significatives d'aigües subterrànies.
, Groundwater is the water present beneath E … Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in the fractures of rock formations. About 30 percent of all readily available freshwater in the world is groundwater. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from the surface; it may discharge from the surface naturally at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology. Typically, groundwater is thought of as water flowing through shallow aquifers, but, in the technical sense, it can also contain soil moisture, permafrost (frozen soil), immobile water in very low permeability bedrock, and deep geothermal or oil formation water. Groundwater is hypothesized to provide lubrication that can possibly influence the movement of faults. It is likely that much of Earth's subsurface contains some water, which may be mixed with other fluids in some instances. Groundwater is often cheaper, more convenient and less vulnerable to pollution than surface water. Therefore, it is commonly used for public water supplies. For example, groundwater provides the largest source of usable water storage in the United States, and California annually withdraws the largest amount of groundwater of all the states. Underground reservoirs contain far more water than the capacity of all surface reservoirs and lakes in the US, including the Great Lakes. Many municipal water supplies are derived solely from groundwater. Over 2 billion people rely on it as their primary water source worldwide. Use of groundwater has related environmental issues. For example, polluted groundwater is less visible and more difficult to clean up than pollution in rivers and lakes. Groundwater pollution most often results from improper disposal of wastes on land. Major sources include industrial and household chemicals and garbage landfills, excessive fertilizers and pesticides used in agriculture, industrial waste lagoons, tailings and process wastewater from mines, industrial fracking, oil field brine pits, leaking underground oil storage tanks and pipelines, sewage sludge and septic systems. Additionally, groundwater is susceptible to saltwater intrusion in coastal areas and can cause land subsidence when extracted unsustainably, leading to sinking cities (like Bangkok)) and loss in elevation (such as the multiple meters lost in the Central Valley of California). These issues are made more complicated by sea level rise and other changes caused by climate changes which will affect the water cycle.changes which will affect the water cycle.
, Grondwater is al het water dat zich in de … Grondwater is al het water dat zich in de ondergrond, in bodems en gesteenten bevindt. Meestal is dit water afkomstig van neerslag, nadat het op de oppervlakte is beland infiltreert het direct of indirect (na zich eerst in meren of rivieren te hebben bevonden). Grondwater afkomstig van neerslag wordt meteorisch water genoemd. Andere bronnen van grondwater zijn het vrijkomen van water bij metamorfe reacties in de diepere delen van de aardkorst of het vrijkomen van water bij het omhoogkomen van magma.n van water bij het omhoogkomen van magma.
, Podzemní voda je voda, která se nachází po … Podzemní voda je voda, která se nachází pod zemským povrchem, zejména v pórech mezi částicemi půdy a v místech, kde je narušena kontinuita hornin. Podzemní vodou je i voda ve studních, ve vrtech, či voda vyvěrající z pramenů. Z pohledu geologického, resp. hydrogeologického, jde o vodu pod zemským povrchem, v nasycené zóně, kde vyplňuje všechny dutiny a je ohraničena svým horizontem. Ostatní vody pod povrchem, které této definici neodpovídají, jsou vody podpovrchové. Patří do nich půdní vlhkost, vody v nenasycené zóně, vody v jiném skupenství i kapilární voda. Výzkumem podzemní vody se zabývá hydrogeologie. Podzemní voda tvoří okolo 20 % dostupných světových zásob sladké vody, využívá se často jako zdroj pitné i užitkové vody. Podzemní voda je nejspolehlivějším zdrojem vody, proces jejího doplňování je však zdlouhavý a závislý na počtu a intenzitě srážek. Proto existuje hrozba, že zásoby podzemní vody budou v některých oblastech dosud zvyklých na určitý stav podzemní vody s pokračující změnou globálního klimatu ubývat. Pokud obsah rozpuštěných minerálních látek nebo plynů překročí stanovenou hranici, označuje se tato voda jako minerální voda; opakem je prostá podzemní voda.ální voda; opakem je prostá podzemní voda.
, Em geologia considera-se água subterrânea … Em geologia considera-se água subterrânea toda aquela água que ocupa todos os espaços vazios de uma formação geológica, os chamados aquíferos. As águas subterrâneas são formadas pelo excedente das águas das chuvas. Nem toda água que está embaixo da terra é considerada como água subterrânea por haver uma distinção daquela que ocupa o lençol freático, que é chamada de água de solo e tem maior interesse para a agronomia e botânica. Um maciço rochoso ou um solo argiloso, pode servir de leito para as águas subterrâneas, pois permitem que ela se acumule e elimine todos os espaços vazios do solo. Em geral, as águas subterrâneas são armazenadas ou em rochas sedimentares porosas e permeáveis, ou em rochas não-porosas, mas fraturadas. Neste último caso, as fraturas geram um efeito físico similar ao da permeabilidade. Um caso menos frequente é o das rochas , nas quais até mesmo a baixa acidez das águas da chuva é capaz de abrir verdadeiros túneis, por onde flui a água subterrânea. A maior reserva de água doce do mundo se encontra nos glaciares (quase 70 %) seguida pela existente no subsolo (quase 30%), representando esta última cerca de 90% do total de água doce disponível para consumo humano. Uma das maiores reservas de águas subterrâneas do mundo é o famoso Aquífero Guarani, que ocupa o subsolo do nordeste da Argentina, centro-sudoeste do Brasil, noroeste do Uruguai e sudeste do Paraguai. Na Dinamarca, 99% da água consumida pelos seus residentes é extraída de reservatórios subterrâneos. E por esse tipo de reservatório ser facilmente contaminado por agrotóxicos, a agricultura do país é minuciosamente controlada pelo governo. é minuciosamente controlada pelo governo.
, Ως εδαφικό νερό χαρακτηρίζεται ιδιαίτερα τ … Ως εδαφικό νερό χαρακτηρίζεται ιδιαίτερα το νερό που κυκλοφορεί (ή βρίσκεται) υπό την επιφάνεια του εδάφους σε διάφορα ιζηματογενή στρώματα (άμμου, χαλίκων κ.λπ.), στη λεγόμενη . Παλαιότερα ο όρος ταυτιζόταν με το (υπόγεια ύδατα), σήμερα όμως με την εξέλιξη της υδρογεωλογίας και της εξ αυτής ακολουθούμενης κατάταξης, το εδαφικό νερό αποτελεί το πρώτο "στρώμα νερού" των υπογείων υδάτων. πρώτο "στρώμα νερού" των υπογείων υδάτων.
, Air tanah adalah semua air yang berada di … Air tanah adalah semua air yang berada di dalam ruang batuan dasar yang mengalir secara alami ke permukaan tanah melalui pancaran atau rembesan. Sumber utama dari air tanah yaitu air hujan yang meresap ke dalam tanah. Peresapan air hujan ini terjadi selama pengaliran air hujan ke laut atau ke aliran sungai. Jumlah resapan air ke dalam tanah ditentukan oleh faktor ruang, waktu, kecuraman lereng, bahan penyusun permukaan tanah dan jenis serta banyaknya vegetasi dan curah hujan. Peran utama air tanah adalah sebagai sumber daya alam terbarukan dan sumber daya air yang menyediakan pasokan air untuk memenuhi berbagai keperluan manusia. Perilaku masyarakat dalam memanfaatkan dan memelihara sanitasi lingkungan sangat mempengaruhi kondisi air didalam tanah.at mempengaruhi kondisi air didalam tanah.
, Les eaux souterraines sont toutes les eaux … Les eaux souterraines sont toutes les eaux se trouvant sous la surface du sol, dans la zone de saturation et en contact direct avec le sol ou le sous-sol. En tant que ressource naturelle vitale et plus ou moins renouvelable et parfois transfrontalières, ces eaux posent des questions juridiques particulières. C'est parfois une source de conflit inter ethnique ou entre pays. Les aquifères souterrains sont la réserve majeure (98 à 99 %)de l'eau douce exploitable sur les terres émergées. L’utilisation de l’eau souterraine se répartit de façon variable d’un pays à l’autre. Les pourcentages d’utilisation, selon les trois catégories, sont les suivants :
* 65 % (0 à 97 %) pour l’irrigation ;
* 25 % (0 à 93 %) pour l'eau potable ;
* 10 % (0 à 64 %) pour l'industrie. La carte des réserves aquifères connues en 2008 (publiée par l'UNESCO) montre 273 aquifères transfrontaliers (68 en Amérique, 38 en Afrique, 65 en Europe de l'Est, 90 en Europe occidentale et 12 en Asie où le recensement n'était pas terminé). Les aquifères majeurs connus en 2008 étaient en Amérique du Sud et Afrique du Nord. Les grands aquifères d'Afrique centrale sont encore mal explorés et rarement exploitées. La multiplication des pompes électriques et petits systèmes de pompage et forage a fortement augmenté la pression sur les nappes, souvent surexploitées dans les zones habitées et de grandes cultures et parfois déjà pollués. Leur exploitation pose aussi des questions sur nos responsabilités à l'égard des générations futures ou de l'amont vers l'aval (du point de vue du sens de circulation des masses d'eau souterraines, ou de leur alimentation via les bassins versants en surface le cas échéant). Il existe des eaux fossiles non renouvelables aux échelles humaines de temps et des aquifères profonds qui ne sont que très lentement réalimentés.ui ne sont que très lentement réalimentés.
, 地下水（英語：Groundwater）顧名思義，就是地面以下的水，是贮存于地面以下岩石裂縫和土壤空隙中的水，按形態分为气态水、吸着水、薄膜水、毛细管水、重力水、固态水等。 地下水一般是硬水，現在可行抽水深度以上水量约为4,200,000立方千米，通过水循环与其他水体交换，在地表下亦緩慢移動。地下水水量稳定，很少受气候影响，污染程度低，可作为居民生活用水、工业用水以及农业灌溉水源。此外，地下水也是生态环境的重要因素和一种活跃的地质营力与信息载体。
, 地下水（ちかすい）とは、広義には地表面より下にある水の総称であり、狭義では、特に地下水面より深い場所では帯水層と呼ばれる地層に水が満たされて飽和しており、このような水だけが「地層水」や「地下水」と呼ばれ、地下水面より浅い場所の水は「土壌水」と呼ばれる。このような狭義では、両者を含めた地表面より下にある水全体は「地中水」と呼ばれる。広義の地下水に対して、河川や湖沼、ため池といった陸上にある水は「表流水」と呼ばれる。
, Wody podziemne – wszystkie wody znajdujące się pod powierzchnią Ziemi.
, Uisce atá i láthair sna carraigeacha póiri … Uisce atá i láthair sna carraigeacha póiriúla cosúil le gaineamhchlocha is aolchlocha. Is féidir go n-éiríonn sé ó uisce a shíothlaigh síos ón dromchla (uisce meitéarach), a bhí ann nuair a leagadh síos an charraig mhoirtiúil (uisce comhaoiseach), nó ó ionsánna doigheartha (uisce nua-ghinte). Tugtar an maoschlár ar an leibhéal faoin talamh a bhfuil na carraigeacha faoina bhun sáithithe le huisce, agus faightear toibreacha nádúrtha mar a sroicheann an maoschlár dromchla an Domhain.oicheann an maoschlár dromchla an Domhain.
, Lurpeko urak lurraren barnera iragazi ondo … Lurpeko urak lurraren barnera iragazi ondoren batekin topo egitean pilatuta geratu diren prezipitazio-urak dira. Lurpeko urek kontinenteetan dagoen ur masaren zati garrantzitsua da. Laku edota ibaietan dagoena baino bolumen handiagoa dute baina glaziarretan dagoena baino txikiagoa. Lurpeko ur masa zabalenek milioika km² izatera iritsi daitezke . Lurpeko urak baliabide garrantzitsuak baina kudeatzeko zailak dira, kutsatuerrazak eta maiz gehiegizko ustiapena sufritzen baitute. Lur gainera erortzen den uraren parte handi samar bat lur gainean labainduz, beheragoko lekuetarantz higitzen da. Hala ere, beste parte bat (lehena bezain garrantzitsua edo garrantzitsuagoa agian), ura doan materialak, porotsua edo apurtua izanik, uzten duen neurrian, zirrikitu edo arrailduretatik sartzen da, eta lur barrenera jaisten da, geruza irazgaitz bat aurkitzen duen arte. Ura metatu egiten da han, behin betiko edo aldi baterako, geruza horren erliebearen eta grabitatearen eraginaren arabera. Lurpeko urek ondorio higatzaileak izaten dituzte, bereziki materialen disoluzioagatik eta arrastatzearen ondorioengatik. Era horretan sortzen dira oro har “” esaten zaien erliebe bereziak. oro har “” esaten zaien erliebe bereziak.
, يحصل الإنسان على احتياجاته المائية من مصدر … يحصل الإنسان على احتياجاته المائية من مصدرين أساسيين وهما مصادر المياه السطحية وتشمل مياه الأنهار والبحيرات ومجاري الوديان ومصادر المياه الأرضية وتشمل الآبار والينابيع والكهوف والدحول. وبالنظر إلى إمكانية مشاهدة المياه السطحية وكذلك بسبب الأموال الباهظة التي صُرِفت على إقامة الخزانات والسدود والقناطر وشق القنوات اللازمة لاستخدام هذه المياه وكلها أمور في كل مكان وفي كل وقت تقريباً لذلك فقد نشأ اعتقاد بأن المياه السطحية تشكل المورد الرئيسي لاحتياجات العالم من المياه ولكن في الواقع فإن أقل من 3% من المياه العذبة المتاحة على كوكب الأرض توجد في الأنهار والبحيرات أما الجزء الأكبر والذي يمثل 97% فإنه يوجد في باطن الأرض ويُقدر بحوالي (100,000) كيلومتر مكعب. وإذا جاز التعبير عن المياه السطحية بأنها في حالة سريان وعبور فإن المصادر الجوفية تمثل المياه في حالة التخزين وقد تجمعت خلال قرون عديدة مع إضافات طفيفة من الأمطار الساقطة سنوياً وبذلك يتضح لنا أهمية المياه الجوفية كمصدر رئيسي يمكن أن يعتمد عليه إذا ما أحسن استغلاله لسد حاجة الإنسان والحيوان والنبات.ويرجع استغلال المياه الجوفية إلى عصور ما قبل الميلاد حيث قام قدماء المصريين والصينيين بحفر الآبار للحصول على المياه من مصادرها الجوفية ولكن لعدم فهم كيفية تواجد المياه وحركتها في باطن الأرض ظل استخدامها محدوداً بل ويكاد يكون محصوراً في بعض المناطق الصحراوية القاحلة والتي لا تتوفر فيها مصادر مياه سطحية. وفي مطلع القرن الحالي ومع التطور الكبير في أدوات الحفر فقد تضافرت عدة جهود لدراسة المياه الجوفية ومنذ ذلك الحين فقد بدأ الاعتماد على المياه الجوفية بشكل ملحوظ خاصة مع تزايد السكان في جميع أنحاء العالم وعدم كفاية المصادر السطحية لتغطية الاحتياجات المائية.المصادر السطحية لتغطية الاحتياجات المائية.
, Grundvatten kallas det vatten som utgör de … Grundvatten kallas det vatten som utgör den underjordiska delen av vattnets kretslopp i naturen. Det bildas genom att nederbörd mycket sakta tränger ner genom marken (infiltration) och sjunker neråt (perkolation). När vattnet når en ogenomtränglig yta (akvifug), exempelvis en sprickfri berghäll av någon kristallin bergart, så magasineras vattnet och fyller ut de hålrum som finns i de lösa jordlagren ovan. Grundvattenytans läge har stor betydelse när man ska gräva brunnar, bygga tunnlar och bergförvar, i jordbruk och i den allmänna samhällsplaneringen. För dricksvattenförsörjning till städer och andra samhällen försöker man så långt som möjligt använda grundvatten. Grundvattenreservoarerna i Sverige finns framförallt i våra rullstensåsar. Grundvattnet kan vara några veckor eller flera tusen år gammalt beroende på akviferernas uppbyggnad och mäktighet. på akviferernas uppbyggnad och mäktighet.
, Підземні води — води, що містяться у верхній частині земної кори. Заповнюють проміжки, пори, тріщини, пустоти, порожнини. У ґрунті заповнюють капіляри. Поділяються на води зони аерації, ґрунтові і артезіанські.
, Grundwasser ist Wasser unterhalb der Erdob … Grundwasser ist Wasser unterhalb der Erdoberfläche, das durch Versickern von Niederschlägen und teilweise auch durch Versickern des Wassers aus Seen und Flüssen dorthin gelangt. Der Gesteinskörper, in dem sich das Grundwasser aufhält und fließt, wird als Grundwasserleiter (aus dem Lateinischen auch: Aquifer, wassertragend bzw. Wasserträger) bezeichnet. Die Fachgebiete, die sich mit Grundwasser befassen, sind die Hydrogeologie und die . Das Gegenstück zum Grundwasser ist das Oberflächenwasser.zum Grundwasser ist das Oberflächenwasser.
, El agua subterránea es agua presente bajo … El agua subterránea es agua presente bajo la superficie terrestre en espacios de rocas o suelos porosos o en los huecos de las formaciones rocosas. Cerca del 30 por ciento de toda el agua dulce disponible en el mundo es agua subterránea. Una acumulación de agua subterránea es considerada un acuífero cuando puede proporcionar una cantidad de agua suficiente para su aprovechamiento por el hombre. La profundidad a la que los espacios de suelo poroso y las grietas o huecos en las rocas están llenos de agua se conoce como nivel freático. El agua subterránea se recarga desde la superficie; puede también salir a la superficie de manera natural a través de manantiales y filtraciones, y puede formar oasis o pantanos. Por otro lado, el agua subterránea se extrae a menudo para su uso en agricultura, industria y consumo humano mediante la construcción de pozos. El estudio de la distribución y movimiento del agua subterránea se denomina hidrogeología. El agua subterránea representa una fracción importante de la masa de agua presente en los continentes, bajo la superficie de la Tierra, tanto en el suelo como en el subsuelo. El volumen del agua subterránea es mucho más importante que la masa de agua retenida en lagos o circulante, y aunque menor que el de los mayores glaciares, las masas más extensas pueden alcanzar un millón o más de km² (como el Acuífero Guaraní). El agua del subsuelo es un recurso importante, y de él se abastece a una tercera parte de la población mundial, pero de difícil gestión, por su sensibilidad a la contaminación y a la sobreexplotación. El agua subterránea es parte de la precipitación que se filtra a través del suelo hasta llegar al material rocoso que está saturado de agua. El agua subterránea se mueve lentamente hacia los niveles bajos, generalmente en ángulos inclinados (debido a la gravedad) y finalmente llega a los arroyos, los lagos y los océanos. Es una creencia común que el agua subterránea llena cavidades y circula por galerías. Sin embargo, no siempre es así, pues puede encontrarse ocupando los intersticios (poros y grietas) del suelo, del sustrato rocoso o del sedimento sin consolidar, los cuales la contienen como una esponja. La única excepción significativa la ofrecen las rocas solubles, como las calizas y los yesos, susceptibles de sufrir el proceso llamado karstificación, en el que el agua excava simas, cavernas y otras vías de circulación, el modelo que más se ajusta a la creencia popular. Un acuífero es una acumulación claramente diferenciada de agua en los poros o grietas de una masa de rocas permeables que permite su circulación. Las rocas almacén pueden ser de materiales muy variados como gravas y areniscas porosas poco cementadas (antiguos sedimentos marinos, de río, playa, eólicos), limos, ciertos tipos de arcilla, calizas agrietadas, e incluso formaciones volcánicas. El nivel superior del agua subterránea se denomina tabla de agua, que en el caso de un acuífero libre corresponde al nivel freático. Es decir, el acuífero consta de una o más capas subterráneas de roca o de otros estratos geológicos que tienen la suficiente porosidad y permeabilidad para permitir ya sea un flujo significativo de aguas subterráneas o la extracción de cantidades significativas de aguas subterráneas.ades significativas de aguas subterráneas.
, Подзе́мные во́ды — воды, находящиеся в толще горных пород верхней части земной коры в жидком, твёрдом и газообразном состоянии.
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Grundakvo estas akvokvanto, kiu sub la ter … Grundakvo estas akvokvanto, kiu sub la tersurfaco formas akvokorpojn en la kavaĵoj (poroj). Ĝi situas super la unua akvoferma tavolo kaj tie plenigas la spacojn inter la grunderoj. La supra nivelo de la grundakvo estas la tersurfaco. La nivelo de la grundakvo en la grundo ŝanĝiĝas depende de la precipitaĵo, temperaturo, aerpremo, laŭ sezono. La normala jara ŝanĝiĝo de grundakvo estas 1-2 metroj. La grundakva nivelo pli-malpli sekvas paralele la geografian surfacon. Ĝi nutras sin el la precipitaĵa akvo kaj malrapide moviĝas al direkto de la deklivo.alrapide moviĝas al direkto de la deklivo.
, Grundvatten kallas det vatten som utgör de … Grundvatten kallas det vatten som utgör den underjordiska delen av vattnets kretslopp i naturen. Det bildas genom att nederbörd mycket sakta tränger ner genom marken (infiltration) och sjunker neråt (perkolation). När vattnet når en ogenomtränglig yta (akvifug), exempelvis en sprickfri berghäll av någon kristallin bergart, så magasineras vattnet och fyller ut de hålrum som finns i de lösa jordlagren ovan. Grundvattenytans läge har stor betydelse när man ska gräva brunnar, bygga tunnlar och bergförvar, i jordbruk och i den allmänna samhällsplaneringen. För dricksvattenförsörjning till städer och andra samhällen försöker man så långt som möjligt använda grundvatten. Grundvattenreservoarerna i Sverige finns framförallt i våra rullstensåsar. Grundvattnet kan vara några veckor eller flera tusenet kan vara några veckor eller flera tusen
, Ως εδαφικό νερό χαρακτηρίζεται ιδιαίτερα τ … Ως εδαφικό νερό χαρακτηρίζεται ιδιαίτερα το νερό που κυκλοφορεί (ή βρίσκεται) υπό την επιφάνεια του εδάφους σε διάφορα ιζηματογενή στρώματα (άμμου, χαλίκων κ.λπ.), στη λεγόμενη . Παλαιότερα ο όρος ταυτιζόταν με το (υπόγεια ύδατα), σήμερα όμως με την εξέλιξη της υδρογεωλογίας και της εξ αυτής ακολουθούμενης κατάταξης, το εδαφικό νερό αποτελεί το πρώτο "στρώμα νερού" των υπογείων υδάτων. πρώτο "στρώμα νερού" των υπογείων υδάτων.
, El agua subterránea es agua presente bajo … El agua subterránea es agua presente bajo la superficie terrestre en espacios de rocas o suelos porosos o en los huecos de las formaciones rocosas. Cerca del 30 por ciento de toda el agua dulce disponible en el mundo es agua subterránea. Una acumulación de agua subterránea es considerada un acuífero cuando puede proporcionar una cantidad de agua suficiente para su aprovechamiento por el hombre. La profundidad a la que los espacios de suelo poroso y las grietas o huecos en las rocas están llenos de agua se conoce como nivel freático. El agua subterránea se recarga desde la superficie; puede también salir a la superficie de manera natural a través de manantiales y filtraciones, y puede formar oasis o pantanos. Por otro lado, el agua subterránea se extrae a menudo para su uso en agricultura, trae a menudo para su uso en agricultura,
, 地下水（英語：Groundwater）顧名思義，就是地面以下的水，是贮存于地面以下岩石裂縫和土壤空隙中的水，按形態分为气态水、吸着水、薄膜水、毛细管水、重力水、固态水等。 地下水一般是硬水，現在可行抽水深度以上水量约为4,200,000立方千米，通过水循环与其他水体交换，在地表下亦緩慢移動。地下水水量稳定，很少受气候影响，污染程度低，可作为居民生活用水、工业用水以及农业灌溉水源。此外，地下水也是生态环境的重要因素和一种活跃的地质营力与信息载体。
, Podzemní voda je voda, která se nachází po … Podzemní voda je voda, která se nachází pod zemským povrchem, zejména v pórech mezi částicemi půdy a v místech, kde je narušena kontinuita hornin. Podzemní vodou je i voda ve studních, ve vrtech, či voda vyvěrající z pramenů. Z pohledu geologického, resp. hydrogeologického, jde o vodu pod zemským povrchem, v nasycené zóně, kde vyplňuje všechny dutiny a je ohraničena svým horizontem. Ostatní vody pod povrchem, které této definici neodpovídají, jsou vody podpovrchové. Patří do nich půdní vlhkost, vody v nenasycené zóně, vody v jiném skupenství i kapilární voda. Výzkumem podzemní vody se zabývá hydrogeologie. Podzemní voda tvoří okolo 20 % dostupných světových zásob sladké vody, využívá se často jako zdroj pitné i užitkové vody.se často jako zdroj pitné i užitkové vody.
, Les eaux souterraines sont toutes les eaux … Les eaux souterraines sont toutes les eaux se trouvant sous la surface du sol, dans la zone de saturation et en contact direct avec le sol ou le sous-sol. En tant que ressource naturelle vitale et plus ou moins renouvelable et parfois transfrontalières, ces eaux posent des questions juridiques particulières. C'est parfois une source de conflit inter ethnique ou entre pays.
* 65 % (0 à 97 %) pour l’irrigation ;
* 25 % (0 à 93 %) pour l'eau potable ;
* 10 % (0 à 64 %) pour l'industrie.ble ;
* 10 % (0 à 64 %) pour l'industrie.
, Em geologia considera-se água subterrânea … Em geologia considera-se água subterrânea toda aquela água que ocupa todos os espaços vazios de uma formação geológica, os chamados aquíferos. As águas subterrâneas são formadas pelo excedente das águas das chuvas. Nem toda água que está embaixo da terra é considerada como água subterrânea por haver uma distinção daquela que ocupa o lençol freático, que é chamada de água de solo e tem maior interesse para a agronomia e botânica. Um maciço rochoso ou um solo argiloso, pode servir de leito para as águas subterrâneas, pois permitem que ela se acumule e elimine todos os espaços vazios do solo.e elimine todos os espaços vazios do solo.
, 지하수(地下水, 문화어: 땅속물)는 지표면 밑을 흐르는 물을 이르는 말이다. … 지하수(地下水, 문화어: 땅속물)는 지표면 밑을 흐르는 물을 이르는 말이다. 지구의 외부는 암석으로 이루어진 지각으로 덮여있고, 식물이 자라는 지표면 바로 밑에는 암석을 관통하여 물이 흐르고 있다. 대부분의 지하수는 흙 속으로 스며든 비와 눈이 녹은 물이 모여서 형성된다. 물은 암석에 도달하면 암석 사이의 열려 있는 틈을 통해 흐른다. 지하수가 흐르는 속도는 지하의 환경에 따라 일정하지 않아서 하루평균 1.5m 정도로 흐르는 곳도 있지만, 어떤 곳의 지하수는 연평균 약 1.5m의 속도로 아주 천천히 흐르기도 한다.어떤 곳의 지하수는 연평균 약 1.5m의 속도로 아주 천천히 흐르기도 한다.
, Wody podziemne – wszystkie wody znajdujące się pod powierzchnią Ziemi.
, Groundwater is the water present beneath E … Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in the fractures of rock formations. About 30 percent of all readily available freshwater in the world is groundwater. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from the surface; it may discharge from the surface naturally at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology,d movement of groundwater is hydrogeology,
, Подзе́мные во́ды — воды, находящиеся в толще горных пород верхней части земной коры в жидком, твёрдом и газообразном состоянии.
, Grundwasser ist Wasser unterhalb der Erdob … Grundwasser ist Wasser unterhalb der Erdoberfläche, das durch Versickern von Niederschlägen und teilweise auch durch Versickern des Wassers aus Seen und Flüssen dorthin gelangt. Der Gesteinskörper, in dem sich das Grundwasser aufhält und fließt, wird als Grundwasserleiter (aus dem Lateinischen auch: Aquifer, wassertragend bzw. Wasserträger) bezeichnet. Die Fachgebiete, die sich mit Grundwasser befassen, sind die Hydrogeologie und die . Das Gegenstück zum Grundwasser ist das Oberflächenwasser.zum Grundwasser ist das Oberflächenwasser.
, Підземні води — води, що містяться у верхній частині земної кори. Заповнюють проміжки, пори, тріщини, пустоти, порожнини. У ґрунті заповнюють капіляри. Поділяються на води зони аерації, ґрунтові і артезіанські.
, Air tanah adalah semua air yang berada di … Air tanah adalah semua air yang berada di dalam ruang batuan dasar yang mengalir secara alami ke permukaan tanah melalui pancaran atau rembesan. Sumber utama dari air tanah yaitu air hujan yang meresap ke dalam tanah. Peresapan air hujan ini terjadi selama pengaliran air hujan ke laut atau ke aliran sungai. Jumlah resapan air ke dalam tanah ditentukan oleh faktor ruang, waktu, kecuraman lereng, bahan penyusun permukaan tanah dan jenis serta banyaknya vegetasi dan curah hujan. Peran utama air tanah adalah sebagai sumber daya alam terbarukan dan sumber daya air yang menyediakan pasokan air untuk memenuhi berbagai keperluan manusia. Perilaku masyarakat dalam memanfaatkan dan memelihara sanitasi lingkungan sangat mempengaruhi kondisi air didalam tanah.at mempengaruhi kondisi air didalam tanah.
, 地下水（ちかすい）とは、広義には地表面より下にある水の総称であり、狭義では、特に地下水面より深い場所では帯水層と呼ばれる地層に水が満たされて飽和しており、このような水だけが「地層水」や「地下水」と呼ばれ、地下水面より浅い場所の水は「土壌水」と呼ばれる。このような狭義では、両者を含めた地表面より下にある水全体は「地中水」と呼ばれる。広義の地下水に対して、河川や湖沼、ため池といった陸上にある水は「表流水」と呼ばれる。
, Grondwater is al het water dat zich in de … Grondwater is al het water dat zich in de ondergrond, in bodems en gesteenten bevindt. Meestal is dit water afkomstig van neerslag, nadat het op de oppervlakte is beland infiltreert het direct of indirect (na zich eerst in meren of rivieren te hebben bevonden). Grondwater afkomstig van neerslag wordt meteorisch water genoemd. Andere bronnen van grondwater zijn het vrijkomen van water bij metamorfe reacties in de diepere delen van de aardkorst of het vrijkomen van water bij het omhoogkomen van magma.n van water bij het omhoogkomen van magma.
, Lurpeko urak lurraren barnera iragazi ondo … Lurpeko urak lurraren barnera iragazi ondoren batekin topo egitean pilatuta geratu diren prezipitazio-urak dira. Lurpeko urek kontinenteetan dagoen ur masaren zati garrantzitsua da. Laku edota ibaietan dagoena baino bolumen handiagoa dute baina glaziarretan dagoena baino txikiagoa. Lurpeko ur masa zabalenek milioika km² izatera iritsi daitezke . Lurpeko urak baliabide garrantzitsuak baina kudeatzeko zailak dira, kutsatuerrazak eta maiz gehiegizko ustiapena sufritzen baitute.iz gehiegizko ustiapena sufritzen baitute.
, L'aigua subterrània representa una fracció … L'aigua subterrània representa una fracció important de la massa de aigua present en els continents, sota la superfície de la Terra, tant en el sòl com en el subsòl ja que, convencionalment, el terme inclou cert espessor com s'assenyala en l'article respectiu, en ser un concepte tridimensional. Evidentment, si solament fos bidimensional no podríem parlar d'aigua subterrània. El volum de l'aigua subterrània és molt més important que la massa d'aigua retinguda en llacs o circulant, i encara que menor al dels majors glacials, les masses més extenses poden aconseguir un milió o més de quilòmetres quadrats (com l'Aqüífer Guaraní). L'aigua del subsòl és un recurs important i d'aquest es proveeix a una tercera part de la població mundial, però de difícil gestió, per la seva sensibilitat a la con gestió, per la seva sensibilitat a la con
, Uisce atá i láthair sna carraigeacha póiri … Uisce atá i láthair sna carraigeacha póiriúla cosúil le gaineamhchlocha is aolchlocha. Is féidir go n-éiríonn sé ó uisce a shíothlaigh síos ón dromchla (uisce meitéarach), a bhí ann nuair a leagadh síos an charraig mhoirtiúil (uisce comhaoiseach), nó ó ionsánna doigheartha (uisce nua-ghinte). Tugtar an maoschlár ar an leibhéal faoin talamh a bhfuil na carraigeacha faoina bhun sáithithe le huisce, agus faightear toibreacha nádúrtha mar a sroicheann an maoschlár dromchla an Domhain.oicheann an maoschlár dromchla an Domhain.
, يحصل الإنسان على احتياجاته المائية من مصدر … يحصل الإنسان على احتياجاته المائية من مصدرين أساسيين وهما مصادر المياه السطحية وتشمل مياه الأنهار والبحيرات ومجاري الوديان ومصادر المياه الأرضية وتشمل الآبار والينابيع والكهوف والدحول. وبالنظر إلى إمكانية مشاهدة المياه السطحية وكذلك بسبب الأموال الباهظة التي صُرِفت على إقامة الخزانات والسدود والقناطر وشق القنوات اللازمة لاستخدام هذه المياه وكلها أمور في كل مكان وفي كل وقت تقريباً لذلك فقد نشأ اعتقاد بأن المياه السطحية تشكل المورد الرئيسي لاحتياجات العالم من المياه ولكن في الواقع فإن أقل من 3% من المياه العذبة المتاحة على كوكب الأرض توجد في الأنهار والبحيرات أما الجزء الأكبر والذي يمثل 97% فإنه يوجد في باطن الأرض ويُقدر بحوالي (100,000) كيلومتر مكعب. وإذا جاز التعبير عن المياه السطحية بأنها في حالة سريان وعبور فإن المصادر الجوفية تمثل المياه في حالة التخزين وقد تجمعت خلال قرون عديدة مع إضاف التخزين وقد تجمعت خلال قرون عديدة مع إضاف
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| rdfs:label |
地下水
, Agua subterránea
, Grundvatten
, Eau souterraine
, Подземные воды
, Groundwater
, مياه جوفية
, Air tanah
, Podzemní voda
, Grundwasser
, Água subterrânea
, 지하수
, Підземні води
, Aigua subterrània
, Grundakvo
, Screamhuisce
, Wody podziemne
, Εδαφικό νερό
, Lurpeko ura
, Grondwater
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