TW201631243A - Technical balance for underground water level system - Google Patents

Technical balance for underground water level system Download PDF

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TW201631243A
TW201631243A TW105116050A TW105116050A TW201631243A TW 201631243 A TW201631243 A TW 201631243A TW 105116050 A TW105116050 A TW 105116050A TW 105116050 A TW105116050 A TW 105116050A TW 201631243 A TW201631243 A TW 201631243A
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groundwater
water
layer
surface water
well
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TW105116050A
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TWI596257B (en
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黃垤樹
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黃垤樹
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Abstract

Technical balance for underground water level system, its technical structure is a human-based technology to accelerate the reduction of the original presence of natural water in the environment, so it can facilitate humans to use water more convenient, and prevent arising disasters from creeks, rivers or low-lying and where theres water in the surface. The surface water and groundwater can link together, by drilling wells and penetrating deep aquifers so that the surface water can quickly go into the underground aquifer storage and can add a large number to the underground aquifer to prevent subsidence and during the dry season, can use a moderate extraction in order to prevent a disaster caused by droughts.

Description

地下水位平衡系統之技術結構 Technical structure of groundwater level balance system

本發明為地下水位平衡系統之技術結構,包括使地面水用滲透井方式與地下水層(地下儲水層)直接連結,讓地面水能快速滲入各地下水層,也就是儲水層,將雨季過剩之地面水直接由滲透井大量滲透儲存於各地下水層儲水,藉以補充地下儲水層被抽取的地下水,提升地下水之水位,預防地層下陷,並備乾季時能被適量抽取使用,而不致有地層下陷之問題,又可解決乾旱之窘境。 The invention is a technical structure of a groundwater level balance system, which comprises directly connecting the surface water with a permeation well method and a groundwater layer (underground water storage layer), so that the surface water can rapidly infiltrate into the groundwater layer, that is, the water storage layer, and the rainy season is surplus. The surface water is directly infiltrated by the permeate well and stored in the groundwater layer to supplement the groundwater extracted from the underground aquifer, raise the water level of the groundwater, prevent the formation from subsiding, and can be used for proper amount during the dry season. The problem of subsidence of the stratum can solve the dilemma of drought.

原始水生態循環是地面的水部分蒸發到天空構成雲,雲轉為雨滴落到地面而成對流雨,另一部分由土壤吸收,經過泥土層滲入,緩慢滲入地下水層(地下儲水層),成為地下水,早期人類掘井取水使用,又成為地面水。海平面的水蒸發到天空,同樣構成雲,雲轉為雨滴落到海面而成對流雨,不論地面或海面被蒸發的水到天空成為雲,隨氣流鋒面漂移到其他地區落下,成為氣流雨,雨水若落在山上,被山上的林木土壤吸收後再緩慢釋放構成泉水,泉水匯集成溪或河,流至平地被人取用,剩餘下至大海,成為非常自然的水生態循環。 The original water ecological cycle is that the water part of the ground evaporates into the sky to form a cloud, the cloud turns into raindrops and falls to the ground to form convective rain, and the other part is absorbed by the soil. After infiltration through the soil layer, it slowly infiltrates into the groundwater layer (underground water storage layer) and becomes Groundwater, used by early human digging wells to take water, has become surface water. The water at sea level evaporates into the sky, which also constitutes a cloud. The cloud turns into a convective rain when the raindrops fall to the surface of the sea. Whether the water on the ground or the surface of the sea is evaporated into the sky becomes a cloud, drifting with the airflow front to other areas, becoming airflow rain. If the rain falls on the mountain, it is absorbed by the forest soil on the mountain and then slowly released to form a spring water. The spring water is collected into a stream or a river, and it is taken to the flat land and taken to the sea. It becomes a very natural water ecological cycle.

為解決澇旱問題,就應將雨季過多的水量,盡量保留,以備乾旱時使用,以往均以建築水庫儲水解決,但目前築水庫,不僅選址困難,又經常遭受人民抗爭,無法建築,再以水庫容易淤積,清除不易,儲水量日減,造成今日難以解決的問題,更因地球環境改變,氣候異常,澇旱嚴重,災害頻傳,此為目前各國政府最頭疼的問題。 In order to solve the problem of drought, the amount of water in the rainy season should be kept as much as possible for use in drought. In the past, water storage in building reservoirs was used to solve the problem. However, at present, the reservoirs are not only difficult to locate but often suffer from people’s struggle and cannot be built. Moreover, the reservoir is easy to accumulate, the removal is not easy, and the water storage is diminishing, causing problems that are difficult to solve today. Moreover, due to changes in the global environment, climate anomalies, severe droughts and frequent disasters, this is the most difficult problem for governments at present.

目前既然無法建水庫,只好另尋能儲水的地方,目前未被人類 想到的地方就是地下水庫,地下水庫就是地下儲水層,也就是地下水層,自古以來缺水地區都鑿開口井,以人力取水使用,後來是鑿井埋管,以人力抽取地下水使用,現在是以馬達抽取使用,都是自地下水層抽取的水,卻可以連續不斷的抽取,而不致斷水,可見其儲水量之多,雖有一小部份抽久會沒水,這就表示水層不夠厚,不夠大。地下水儲水之空間非常大,目前大家知道抽取使用,也知道地下水必須由地面水經土壤層的回滲,但未想到以人力改變滲透的方式,使地面水直接滲入地下水層,提高滲透速度,快速補充地下水,因此若能攫取雨季過多的乾淨水儲存於地下水層,提高地下水位,作為地下水來源,乾季時就可適度抽取使用。地下水層是由上往下多層分布,分為淺層與深層,數十公尺深的叫淺層,淺層又有許多層,數百公尺深的叫深層,深層也有許多層。為什麼抽取深層地下水層的地下水會對地層下陷影響較嚴重,抽取淺層地下水層的地下水影響比較輕,因為目前之地下水是由地表的地面水經土壤回滲進入地下,深層地下水層因為比較深,補充較慢,且經土壤之回滲速度緩慢,再加上人口聚集,透水面積一直減少,抽水速度又一直增加,所以地下水無法充分補足,使地下水層產生空隙,該空隙在水無法即時補充的情況下,便會逐漸被壓縮,導致地層緩慢下沈。深層地下水層之地下水被抽取後,便由淺層之地下水層的地下水往下滲透補充,但補充速度有限,且深層水井口徑大,抽水量多,需要快速大量的補充,但不易補足,且在補充過程又導致淺層地下水流失,淺層流失之地下水再由地表水回滲補充,在這補充過程,深層地下水之補充比淺層慢,所以其影響地層下陷較大。又在回滲之過程,土壤含水層的水也會因乾季,地表水回滲少而流失,含水層之土壤也會壓縮,且乾季抽水量也較大,在這種惡性循環下,地層下陷會更快速嚴重。當地下水被抽取後,儲水的地下水之砂石會產生空隙,土壤含水層之水位下降也會產生空隙,當空隙產生後,如果沒 有水補充,該等空隙便會逐漸被壓縮,當空隙被壓縮後,有水補充也無法再恢復,這樣不僅地層下陷,儲水空間被壓縮,儲水量便會減少,以後再補充,便不會產生作用。依據監察院99年9月調查報告及工研院彰雲地區長期地層監測資料,該地區地層下陷主要來自深層(200公尺以下)地層的壓縮,主要為深水井之抽用,一般農業用水只抽取淺層地下水(30公尺以上),農民灌溉水井抽水對地層下陷影響相對輕微,政府為解決地層下陷,研擬「雲彰黃金廊道農業新方案」做為「黃金十年-樂活農業」的旗艦示範區,以三新二節新動能-「新技術、新農民、新產業」為策略目標,於102至109年期間將投資33億元打造「節水、節能」的農業黃金廊道,但地層下陷不僅只有雲彰地區。 At present, since it is impossible to build a reservoir, it has to find another place where water can be stored. The place of thought is the underground reservoir. The underground reservoir is the underground water storage layer, which is the groundwater layer. Since the ancient times, the water-deficient areas have been used to open the wells, and the manpower is used for water. Later, the wells are buried and the groundwater is used for manpower extraction. Now The motor is extracted from the groundwater layer, but it can be continuously extracted without breaking the water. It can be seen that there is a large amount of water stored. Although there is a small amount of water for a long time, it means that the water layer is not enough. Thick, not big enough. The space for groundwater storage is very large. At present, we know that it is used for extraction. It is also known that groundwater must be oozing from the surface water through the soil layer. However, it is not expected that the groundwater will be directly infiltrated into the groundwater layer by man-made infiltration, and the penetration speed will be increased. Quickly replenish groundwater, so if you can take too much clean water in the rainy season and store it in the groundwater layer, raise the groundwater level and use it as a groundwater source for moderate use during the dry season. The groundwater layer is distributed from top to bottom, divided into shallow and deep layers. The shallow layer is called tens of meters deep, and there are many layers in the shallow layer. The depth is hundreds of meters deep and there are many layers in the deep layer. Why the groundwater in the deep groundwater layer will have a serious impact on the subsidence of the stratum, and the groundwater in the shallow groundwater layer will be less affected, because the groundwater from the surface is back to the ground through the soil, and the deep groundwater layer is deeper. The replenishment is slow, and the rate of re-infiltration through the soil is slow. Together with the population accumulation, the permeable area has been reduced and the pumping speed has been increasing. Therefore, the groundwater cannot be fully replenished, causing the groundwater layer to create a gap, which cannot be immediately replenished in the water. In this case, it will gradually be compressed, causing the formation to sink slowly. After the groundwater in the deep groundwater layer is extracted, it will be infiltrated and supplemented by the groundwater in the shallow groundwater layer, but the replenishing speed is limited, and the deep water well has a large caliber and a large amount of pumping. It needs a quick and large amount of replenishment, but it is not easy to make up, and The replenishment process leads to the loss of shallow groundwater. The shallow groundwater is replenished by surface water re-infiltration. In this supplementary process, the deep groundwater replenishment is slower than the shallow layer, so it affects the stratum depression. In the process of re-infiltration, the water in the soil aquifer will also be lost due to the dry season, less surface water re-infiltration, the soil in the aquifer will also be compressed, and the amount of water pumped in the dry season will be larger. Under this vicious cycle, the stratum subsidence It will be more serious and serious. When the groundwater is extracted, the sandstone of the groundwater that stores the water will create a gap, and the water level of the soil aquifer will also produce a gap. When the gap is generated, if With water replenishment, the gaps will be gradually compressed. When the gap is compressed, water can not be recovered again. This will not only reduce the formation, the storage space will be compressed, and the water storage will be reduced. Will have a role. According to the investigation report of the Institute of Supervision in September 1999 and the long-term ground monitoring data of the Zhangye area of the Industrial Engineering Research Institute, the depression of the stratum in the area mainly comes from the compression of deep (200 meters below) strata, mainly for the extraction of deep water wells. Extracting shallow groundwater (above 30 meters), the impact of pumping irrigation by farmers on irrigation wells is relatively minor. To solve the problem of subsidence, the government has developed a new “Golden Golden Corridor Agriculture Plan” as “Golden Decade-Live Agriculture”. The flagship demonstration zone is based on the new kinetic energy of the new and new developments - "new technologies, new farmers, new industries". It will invest 3.3 billion yuan in the period of 102-109 to create a water-saving and energy-saving agricultural gold corridor. However, the formation subsidence is not only the Yunzhang area.

內政部建築研究所力推養生池、透水鋪面等滲透方法,也是原始水生態循環的一環,只是現在建築,除建築面積被鋪上不透水鋪面外,其法定空地也被鋪上不透水鋪面,如水泥等,所以在建築技術規則規定法定空地必須是透水鋪面,以增加透水鋪面的面積,增加雨天地面之透水量,但在台灣人民之土地使用觀念,寸土寸金,哪有可能讓土地閒置,因此當建築物驗收完成後,立即被鋪上不透水鋪面,作為其他用途,因此該規定毫無效果。養生池如同目前政府所建立的蓄洪池,蓄洪池僅作為防洪功能,晴天就恢復為一般透水鋪面,成為市民活動空間,回滲效果有限,也失去養生池應有的功能,因為市區土地昂貴,空間不足,沒有多餘土地可做為養生池。 The Institute of Building Research of the Ministry of the Interior promotes infiltration methods such as health pools and permeable pavements. It is also part of the original water ecological cycle. It is only the current building. In addition to the construction area being covered with impervious pavement, its legal open space is also covered with impervious pavement. Such as cement, etc., in the construction technical rules, the statutory open space must be permeable pavement to increase the area of permeable pavement and increase the amount of water permeated on the rainy day. However, in the land use concept of the people of Taiwan, it is possible to leave the land idle. Therefore, when the building is completed, it is immediately covered with impervious paving for other purposes, so the rule has no effect. The health pool is like the flood storage pond established by the government. The flood storage pond is only used as a flood control function. On sunny days, it will return to the general permeable pavement and become a space for citizens to live. The effect of re-infiltration is limited and the function of the health pool is lost. Insufficient space, no surplus land can be used as a health pool.

貴局提供之檢索資料「滲透井保水系統設計施工」,仍然脫離不了自然的水生態循環的基本原理,它雖然設有滲透井,井深也不過在1米內,並未穿透土壤層到達地下水層,且因土壤性質不同,滲透率有非常大之差異,仍然須透過土壤層往下滲透,其滲透管,只是增加其滲透面積,滲透速度仍然受土壤之 滲透速度所束縛,其設計是要增加雨水之留置量及滲透時間與滲透面積,雖有其某種程度之效果,較建築研究所之透水鋪面進步,但速度仍不足以完全補足地下水層之水位,又易受環境之影響,也會促使有土壤液化地區之液化情況加重。  The search data provided by your office, "Design and Construction of Infiltration Well Water Conservation System", still cannot escape the basic principle of natural water ecological cycle. Although it has an infiltration well, the well depth is within 1 meter and does not penetrate the soil layer to reach groundwater. Layer, and due to different soil properties, the permeability is very different, still has to penetrate through the soil layer, its permeation tube only increases its permeate area, and the penetration rate is still affected by the soil. The osmotic speed is bound, and its design is to increase the amount of rainwater retention and penetration time and permeation area. Although it has some effect, it is better than the permeable pavement of the Institute of Architecture, but the speed is still not enough to fully fill the water level of the groundwater layer. It is also susceptible to the environment and will also contribute to the liquefaction of soil liquefaction areas.

貴局提供之檢索申請案號096213083號塑膠陰井創新組合結構,沒有說明書,由申請專利範圍可確認為一種種植所需之排水系統,目的是在預防植物因土壤排水性不佳,以致會被過剩之水浸泡而使根部腐爛,技術功能結構與本案之地面水回滲地下水層之技術功能結構,毫無關聯。  The innovative application structure of the plastic injection well No. 096213083 provided by your office has no instructions. The scope of the patent application can be confirmed as a drainage system required for planting. The purpose is to prevent plants from being poorly drained due to soil drainage. The excess water is soaked and the roots are rotted. The technical functional structure has nothing to do with the technical functional structure of the surface water infiltration groundwater layer in this case.

貴局提供之檢索申請案號094112762號「軟弱地層壓密沈陷集水管及其使用方法」,同樣沒有說明書,只可判定是建築基礎技術,無法判定是為防止建築地基崩塌或是建築地基土壤之穩固,但由其名稱應是建築地基土壤之穩固,此技術在應用上,防止建築地基崩塌,應用較廣,該技術功能不僅沒有本案之技術功能概念,更與本案之技術功能完全背道而馳。  The search application number No. 094112762 provided by your office, "Weakly laminated and densely sinking water collecting pipe and its use method" also has no specification. It can only be judged as the basic technology of the building. It cannot be judged to prevent the foundation of the building from collapsing or the foundation soil of the building. It is stable, but its name should be the stability of the soil of the building foundation. This technology is applied to prevent the collapse of the building foundation and has a wide application. This technical function not only has no technical function concept of this case, but also runs counter to the technical function of this case.

目前拜科技之賜,都市聚集,工業林立,地表透水面積大量減少,又因科技發達,需水量大量增加,天然循環之供水量嚴重不足,於是大量抽取地下水補充,再加上地球環境改變,導致氣候異常,因此造成地層下陷,暴雨襲擊,以致澇旱頻傳,災害不斷,因此才發明「一種水之生態系統整治結構」,申請案號為100104172號,希能徹底解決澇旱問題,無奈溪流整治與地下水位平衡被 貴局認為是兩個無關之技術,因而分割出「地下水位平衡系統之技術結構」。 At present, thanks to the gift of technology, the city gathers, the industry stands, the surface permeable area is greatly reduced, and because of the advanced technology, the water demand is increasing, and the natural circulation water supply is seriously insufficient. Therefore, a large amount of groundwater replenishment is added, and the earth environment changes, resulting in The climate is abnormal, resulting in the subsidence of the stratum and the heavy rains, resulting in frequent droughts and frequent disasters. Therefore, it was invented that "a water ecosystem remediation structure", application number 100104172, can completely solve the drought problem, helpless stream remediation The balance with the groundwater level is considered by the Bureau to be two unrelated technologies, thus separating the “technical structure of the groundwater level balance system”.

名詞解釋:地下水層,也可稱之為地下儲水層,又可稱之為水脈,水脈猶如礦脈,有深,有淺,有大,有小,但其儲量及空間都很大,宜蘭雪隧隧道開挖時遇上破碎層,湧出大量泉水,那就是水脈,也就是地下水層,因為是在山上,便被稱之為泉水,溪底的儲水層叫伏流水,如果被埋入地底下,就是水脈, 就是地下水層。 Noun explanation: Groundwater layer, also known as underground water storage layer, can also be called water vein, water vein is like a vein, deep, shallow, large, small, but its reserves and space are very large, Yilan Snow When the tunnel is excavated, it encounters a broken layer and a large amount of spring water is poured out. That is the water vein, that is, the groundwater layer. Because it is on the mountain, it is called spring water. The water storage layer at the bottom of the stream is called the effluent water. If it is buried Underneath, it’s the water veins. It is the groundwater layer.

若要徹底解決上述問題,唯一方法就是使用本發明之地下水位平衡系統之技術結構,以人為力量,使地面水不經過土壤層滲透,能快速直接滲透補充地下各水層,使地下水位快速升高,才能有效防止或減緩地層下陷,也就是在有水之地面,鑿滲透井使地面水與地下各水層直接連結,讓地面水能快速補充地下水,使地下水位快速升高;若高處之淺層地下水層與低處之淺層地下水層為同一水層,則在高處使地面水與地下水層連結,低處之地面可能恢復以往由地面冒出的泉水。 The only way to completely solve the above problems is to use the technical structure of the groundwater level balance system of the present invention to artificially make the surface water not penetrate through the soil layer, and to quickly and directly infiltrate and replenish the underground water layers, so that the groundwater level can be rapidly increased. High, in order to effectively prevent or slow down the subsidence of the stratum, that is, in the ground with water, the percolation well is made to directly connect the surface water with the underground water layers, so that the surface water can quickly replenish the groundwater, so that the groundwater level rises rapidly; The shallow groundwater layer is in the same water layer as the shallow groundwater layer in the lower part, and the ground water and the groundwater layer are connected at a high place, and the low ground may restore the spring water emerging from the ground.

本發明之地下水位平衡系統之技術結構,在有水之地面,鑿滲透井使地面水與地下各水層直接連結,滲透井填滿滲透材料,如砂石、透水陶瓷顆粒等,並在地面水之底,鋪一層砂石等滲透材料,讓地面水能由滲透材料之過濾成為乾淨之地面水快速滲到地下水層,因滲透材料有淨化水質作用,使滲入地下水層的水得到淨化效果;滲透井開鑿在河(溪)床上時,滲透井填滿之滲透材料,如砂石、透水陶瓷顆粒等,應填滿至伏流層,與伏流層之砂石密接,這樣溪(河)水就會自然滲入地下水層。在雨季水量多時,為讓地面水回歸地下水層之量增多,速度增快,以減少排入海裡的水量,可以在滲透井中裝入滲透管,滲透管四周同樣填滿滲透材料,如砂石、陶瓷顆粒等,平時是以自然滲透方式,讓地面水經滲透材料滲入地下水層。滲透井之中間放置之滲透管,滲透管因為是中空,可讓乾淨的水直接快速進入井之底部,能快速滲入地下各水層,若要加快速度,則可用人工加壓方式,讓地面水藉壓力大量快速滲入地下水層,大量滲入地下水層的結果,滲入深層地下水層時,深層地下水位上升,地層可能就不致繼續下陷,滲入淺層的地下水層時,淺層的地下水位上升,則往昔的湧泉,可能就會再度出現。 The technical structure of the groundwater level balance system of the invention is that in the ground with water, the percolation well is drilled to directly connect the surface water with the underground water layers, and the permeation well is filled with the infiltration material, such as sandstone, permeable ceramic particles, etc., and is on the ground. At the bottom of the water, a layer of sand and other infiltration materials are laid, so that the surface water can be filtered by the infiltration material to become a clean ground water and quickly infiltrate into the groundwater layer. Because the infiltration material has the function of purifying water, the water infiltrating into the groundwater layer is purified; When the permeate well is cut into the river (stream) bed, the infiltration material filled in the permeate well, such as sandstone and permeable ceramic particles, should be filled to the vortex layer and closely connected with the gravel of the vortex layer, so that the river (river) water It will naturally penetrate into the groundwater layer. In the rainy season, when the amount of water in the rainy season is increased, in order to increase the amount of surface water back to the groundwater layer and increase the speed to reduce the amount of water discharged into the sea, a permeation pipe can be installed in the permeation well, and the permeation pipe is also filled with permeating materials, such as sand and gravel. Ceramic granules, etc., are usually in a natural osmosis manner, allowing surface water to penetrate the groundwater layer through the permeable material. The permeation tube placed in the middle of the infiltration well. Because the permeation tube is hollow, the clean water can be quickly and directly entered into the bottom of the well, and can quickly penetrate into the underground water layers. If the speed is to be increased, the artificial water can be used to make the surface water As a result of a large amount of rapid infiltration into the groundwater layer and a large infiltration into the groundwater layer, the deep groundwater level rises when the deep groundwater layer penetrates, and the formation may not continue to sink. When the shallow groundwater layer penetrates, the shallow groundwater level rises. The springs may reappear.

本發明之地下水位平衡系統之技術結構,再溪(河)床上鑿井,由於地層有許多地下水源層,地下水源層的水是靠地表的 雨水滲透地層,及樹根在下雨時,樹木枝葉吸飽水分後,從樹根的釋出,由於地表環境被破壞,樹木遭砍伐,地表不透水層增加,再加上人類無限制的抽取,致使地下水位下降,水源逐漸枯竭,地層下陷,以往到處可見之泉水已不再復見,目前人類科技發達,為求科技發展及舒適生活,需水孔急,破壞變本加厲,將造成生態浩劫,演變成人類災難,最近氣候異常,如美國全國50州有49州的冰天雪地,澳洲昆士蘭省的水災,中國大陸東南的大雪,台灣88風災小林村的滅村,去年至今,泰國、越南、印度、委內瑞拉的大乾旱,稻田土穰龜裂,農作欠收,委內瑞拉甚至還引發糧食配給,為省電,公務員一週上班兩天,有多嚴重,今年(105年)年初的超級寒流,養殖漁業與農作的損失嚴重,該等天災頻傳,這是生態破壞的結果,因此必須盡速想出對策,避免生態浩劫,不讓天然災害一再繼續發生,又要有足夠之水資源,唯一方法就是將雨季過剩的水資源保留,不讓其快速奔入大海,不泛濫成災,好讓人類利用與生態發展,並防阻地層下陷。所以本發明在築有蓄水壩堤截流河(溪)水,貯存雨水的河(溪)床上鑿滲透井,利用伏流層之天然砂石資源作為過濾材料,並利用乾淨的伏流水大量回歸滲入地下水層,使雨季的溪(河)水大量補充伏流水而留置,當雨季水量充沛時,可用人工加壓方式,藉壓力讓更大量的水能快速滲入地下水層,使地下水位升高,以防阻地層下陷,當缺水時,因地下水位高,也必須適度抽取使用,以達平衡,方便日後的回滲,所以目前使用的水井便可適度抽取井水使用,就不怕抽取而造成地層下陷,這樣就可提供乾旱時之用水,解決水源不足的問題。在都市裡,建築物林立,透水之面積極少,所以建築研究所規定(建築技術規則規定)空地比之空地必須透水鋪面,讓土壤透水,但要滲入到地下水層,非常緩慢,因為建築需要穩固,土壤必須壓實,所以透水不易,否則便易助長土壤液化,況且在建築完成驗收後,大部分被水泥封閉作為其他用途,政府也未徹底執 行,形同虛設,毫無作用,若要用滲透井將雨水直接引入地下水層,由於都市地面水易受汙染,控制不易,若貿然引入地下,地下水易受汙染,反而造成更大災害,但有屋頂之雨水可供利用,由於屋頂之雨水未受汙染,只要簡單過濾塵土,便可得乾淨水源,再直接用滲透井引入地下水層,況且可藉屋頂高度之壓力,讓雨水能更快速滲入地下水層,大量的屋頂雨水未排入排水溝,因此可降低都市水災,並降低改建下水道之財務負擔,且滲透井林立,只要做技術性巧妙之設計,滲透井也可改為取水井與滲透井共用,並於井口設置開關,作為管制,避免超抽。當地下水受汙染時,又可作為監控與復原之設備使用。 The technical structure of the groundwater level balance system of the present invention, the well is drilled on the re-sand (river) bed, because the ground has many groundwater source layers, and the groundwater source layer is water-based. When rainwater penetrates the stratum and the roots of the trees are raining, the leaves and leaves absorb the water, and the roots are released. Because the surface environment is destroyed, the trees are cut down, the surface impervious layer increases, and humans receive unlimited extraction. As a result, the groundwater level has dropped, the water source has gradually dried up, and the stratum has subsided. The springs that have been seen everywhere are no longer seen. At present, human science and technology are developed. In order to seek scientific and technological development and comfortable life, the need for water is urgent and the damage is intensified, which will lead to ecological catastrophe and evolution. Adult disasters, recent climate anomalies, such as 49 states in the United States, 49 states of ice and snow, floods in Queensland, Australia, heavy snow in southeastern China, Taiwan 88 winds in Xiaolin Village, last year, Thailand, Vietnam, India, Venezuela The drought, the cracking of rice fields, the lack of farming, Venezuela even caused food rations, saving electricity, civil servants working two days a week, how serious, the super cold current at the beginning of this year (105 years), farming fisheries and farming The loss is serious, and these natural disasters are frequently transmitted. This is the result of ecological damage. Therefore, we must come up with countermeasures as soon as possible to avoid Holocaust, to prevent natural disasters from continuing to occur, and to have enough water resources, the only way is to retain excess water resources during the rainy season, so that they do not allow them to quickly enter the sea, not flooding into disasters, so that human use and ecological development, And prevent the formation from subsiding. Therefore, the present invention drills a permeate well on a river (stream) bed in which a water storage dam is intercepted and a river (stream) is stored, and the natural sandstone resources of the vortex layer are used as a filter material, and a large amount of reflow water is used to return to the infiltration. The groundwater layer allows the creek (river) water in the rainy season to be filled with a large amount of recharged water. When the rainy season is abundant, artificial pressure can be used to allow a larger amount of water to quickly penetrate into the groundwater layer and raise the groundwater level. The anti-resistance stratum subsides. When there is water shortage, due to the high groundwater level, it must be properly extracted to achieve balance and facilitate future re-infiltration. Therefore, the wells currently used can be properly used for well water extraction, and the formation is not afraid of extraction. Sinking, so that water can be provided during drought to solve the problem of insufficient water. In the city, there are many buildings, and there are few permeable bodies. Therefore, the Institute of Buildings (the rules of the building technology regulations) must be permeable to the open space to allow the soil to be permeable, but it is very slow to penetrate into the groundwater layer because the building needs to be stable. The soil must be compacted, so it is not easy to permeate water, otherwise it will easily promote soil liquefaction. Moreover, after the construction is completed, most of it is closed by cement for other purposes, and the government has not completely implemented it. It is useless, it has no effect. If the infiltration well is used to directly introduce rainwater into the groundwater layer, because the urban surface water is vulnerable to pollution, the control is not easy. If it is introduced into the ground, the groundwater is susceptible to pollution, but it causes more disasters, but has a roof. The rainwater is available for use. Since the rainwater on the roof is not polluted, as long as the dust is simply filtered, the clean water source can be obtained, and the groundwater layer can be directly introduced into the penetrating well. Moreover, the pressure of the roof can be used to allow the rainwater to penetrate into the groundwater layer more quickly. A large amount of roof rainwater is not discharged into the drainage ditch, so it can reduce urban flooding, reduce the financial burden of rebuilding the sewer, and penetrate the wells. As long as the technical ingenious design, the penetrating well can be replaced by the water well and the penetrating well. And set the switch at the wellhead as a regulation to avoid over-pumping. When groundwater is contaminated, it can be used as a monitoring and recovery device.

本發明實施方式以下列實施利說明。 The embodiments of the present invention are described in the following embodiments.

1‧‧‧地面水 1‧‧‧ surface water

2‧‧‧滲透井 2‧‧‧Infiltration well

3‧‧‧地下水層 3‧‧‧ Groundwater layer

4‧‧‧滲透材料 4‧‧‧Infiltration materials

5‧‧‧滲透井地滲透管 5‧‧‧Infiltration wells

6‧‧‧井壁 6‧‧‧ Well wall

7‧‧‧伏流層 7‧‧‧ voltosphere

8‧‧‧滲透管之滲透孔 8‧‧‧Infiltration hole of permeation tube

圖1為低窪有地面水處滲透井之剖面示意圖。 Figure 1 is a schematic cross-sectional view of a percolation well below ground water.

圖2為低窪有地面水處滲透井內有滲透管之剖面示意圖。 Figure 2 is a schematic cross-sectional view of a permeate tube in an infiltration well below ground water.

圖3為溪床上有一層很厚之伏流層7的砂石層之滲透井之剖面示意圖。 Figure 3 is a schematic cross-sectional view of an infiltration well of a sandstone layer having a thick layer of voltaic layer 7 on the stream bed.

圖4為溪床上有一層很厚之伏流層7的砂石層之滲透井內有滲透管之剖面示意圖。 Figure 4 is a schematic cross-sectional view of a permeate tube in a permeate well having a layer of a thick layer of vortex layer 7 on the stream bed.

本發明地下水位平衡系統之技術結構,實施方式以實例說明,如圖1所示,要保留夏季過剩之水資源的方法是於低窪有地面水處1或溪床上有地面水處1鑿滲透井2,深入各地下水層3,滲透井中填滿如砂石或透水陶粒等滲透材料4,使地面水1與地下水層3連結,地面水1由滲透材料4過濾滲透進入地下水層3,將下雨的地面水儲存於地下水層中,這樣可以讓地下水位升高,防阻地層下陷,乾季缺水時可適度抽取使用。滲透井也可連接各種不同來源的水源,如屋頂乾淨的雨水或泉水等,一樣可達成相同之效果;又雨季時雨水變成大量地面水,為使地面水能大量儲存於地下水層,如圖2所示,滲透井中可放入 滲透管5,滲透管5與滲透井2之井壁6間同樣填滿如砂石、透水陶粒等滲透材料4,平常是以自然滲透方式,讓地面水1以自然滲透方式經滲透材料4,滲入地下水層3,若地面水乾淨時,亦可直接進入滲透管5,由滲透管5底部直接經滲透材料4,快速滲入各地下水層3,若要更快速大量使地面水1滲入地下水層3儲存,可藉由人工加壓方式將地面水1經滲透管5,再直接由底部高壓經滲透材料4滲入地下水層3。 The technical structure of the groundwater level balance system of the present invention is illustrated by an example. As shown in FIG. 1 , the method for retaining excess water resources in the summer is to have a surface water at a low level or a surface water at a stream bed. 2, deep into each groundwater layer 3, the permeation well is filled with permeable material 4 such as sandstone or permeable ceramic granules, so that the surface water 1 is connected with the groundwater layer 3, and the surface water 1 is filtered by the permeable material 4 to penetrate into the groundwater layer 3, and the next The ground water of the rain is stored in the groundwater layer, which can raise the groundwater level, prevent the formation from subsiding, and use it moderately in the dry season. The infiltration well can also be connected to water sources of various sources, such as clean rain or spring water on the roof, which can achieve the same effect. In the rainy season, the rainwater becomes a lot of surface water, so that the ground water can be stored in the groundwater layer in large quantities, as shown in Figure 2. As shown, it can be placed in the permeate well The permeate tube 5, the permeate tube 5 and the well wall 6 of the permeate well 2 are also filled with the permeate material 4 such as sandstone and permeable ceramic granules, usually in a natural infiltration manner, so that the surface water 1 penetrates the material in a natural permeation manner. Infiltrated into the groundwater layer 3, if the surface water is clean, it can also directly enter the permeate pipe 5, and the bottom of the permeation pipe 5 directly penetrates the groundwater layer 3 through the permeating material 4, and the groundwater 1 is infiltrated into the groundwater layer more rapidly. 3 Storage, the ground water 1 can be permeated through the permeate tube 5 by manual pressurization, and then directly infiltrated into the groundwater layer 3 through the permeated material 4 from the bottom high pressure.

本發明地下水位平衡系統之技術結構,實施方式中於溪床上鑿滲透井2深入地下水層3時,如圖3所示,溪床上有一層很厚的伏流層7的砂石層,伏流層7的砂石層中有很豐富的水流,就是俗稱的伏流水,該伏流水是最為乾淨的水源,以此伏流水作為滲入地下水層3是最佳之水源,所以滲透井之滲透材料4應填滿與伏流層7的砂石層密接,也可使伏流層7的水能直接滲入滲透管5快速進入地下水層3,伏流水是經過伏流層的砂石過濾,所以滲入地下水層3的水是乾淨的水,雨季水多,則可在未下雨,溪水澄清乾淨時,利用人工加壓,以加速溪水滲入地下水層,將溪(河)水藉由滲透井2之滲透管5滲入到各地下水層儲存,往昔地上湧泉的景象有可能復見,同時可調查該地下水層之分布,在其分布區之範圍內,也可鑿井抽取使用,抽取時注意滲透水量與地下水位,也就不至於有地下水位下降與地層下陷的問題。 The technical structure of the groundwater level balance system of the present invention, in the embodiment, when the percolation well 2 is drilled into the groundwater layer 3 on the stream bed, as shown in Fig. 3, there is a thick gravel layer of the voltaic layer 7 on the stream bed, and the vortex layer 7 There is a very rich water flow in the sandstone layer, which is commonly known as voltaic water. The voltaic water is the cleanest source of water. The effluent water is the best source of water for infiltration into the groundwater layer 3, so the infiltration material 4 of the penetrating well should be filled. Fully connected with the sand layer of the vortex layer 7, the water of the voltaic layer 7 can be directly infiltrated into the permeate tube 5 and quickly enter the groundwater layer 3, and the undulating water is filtered by the gravel of the voltaic layer, so the water infiltrating into the groundwater layer 3 is If the water is clean and there is too much water in the rainy season, it can be used without any rain. When the stream is clear and clean, artificial pressure is applied to accelerate the infiltration of the stream into the groundwater layer, and the river (river) water is infiltrated into each of the permeate tubes 5 of the permeate well 2. The groundwater layer is stored, and the scene of the springs on the ground may be revisited. At the same time, the distribution of the groundwater layer can be investigated. Within the scope of the distribution area, the well can be used for extraction and the amount of water and groundwater level should be paid attention to during the extraction. Not until There is a problem of falling groundwater level and subsidence of the ground.

本發明地下水位平衡系統之技術結構,在市區地面不是柏油、水泥地面,就是建築物,透水面積有限,雨水難以滲入地下,因建築抽水或鑿井取水,容易造成地下水位下降,導致地層下陷。在市區地面水易受汙染,不能引入地下,所以能利用的地面水,就是屋頂之雨水,該雨水經簡單過濾成為乾淨的水,直接連結進入滲透管5,滲入各地下水層,因屋頂離地面有相當之高度,自然形成壓力,能促使雨水加速滲入各地下水層儲存,因此雨季強降雨時,由於屋頂雨水排入地下水層,大量減 輕排水溝及下水道之排水負擔,有降低市區之水災發生,甚至消除水災之功能,因有地面水之補注,地下水位上升,乾季缺水時,便可適度抽取使用,同時可作為市區地下水有無受汙染之監控,由於滲透井遍布,同時也可做為汙染之清除或改善之用途。 The technical structure of the groundwater level balance system of the invention is not tarmac, cement floor or building in the urban area, and the permeable area is limited, and the rainwater is difficult to infiltrate into the ground. Because the building pumping water or sinking the water, it is easy to cause the groundwater level to fall, resulting in the formation subsidence. . In the urban area, the surface water is easily polluted and cannot be introduced into the ground. Therefore, the surface water that can be used is the rainwater on the roof. The rainwater is simply filtered into clean water, directly connected into the permeate pipe 5, and infiltrated into the groundwater layer. The ground has a considerable height and naturally forms pressure, which can promote the accelerated infiltration of rainwater into the groundwater layer. Therefore, when the rain falls during the heavy rain, the roof rainwater is discharged into the groundwater layer, which is greatly reduced. The drainage burden of light drainage ditch and sewerage has the function of reducing the occurrence of floods in urban areas and even eliminating floods. Because of the replenishment of surface water, the groundwater level rises, and when the dry season is short of water, it can be appropriately extracted and used as an urban area. Whether the groundwater is monitored for pollution or not, it can also be used for the removal or improvement of pollution due to the penetration of the well.

1‧‧‧地面水 1‧‧‧ surface water

2‧‧‧滲透井 2‧‧‧Infiltration well

3‧‧‧地下水層 3‧‧‧ Groundwater layer

4‧‧‧滲透材料 4‧‧‧Infiltration materials

5‧‧‧滲透井地滲透管 5‧‧‧Infiltration wells

6‧‧‧井壁 6‧‧‧ Well wall

7‧‧‧伏流層 7‧‧‧ voltosphere

8‧‧‧滲透管之滲透孔 8‧‧‧Infiltration hole of permeation tube

Claims (4)

地下水位平衡系統之技術結構,其特徵在於有地面水處之地面鑽滲透井深入各地下水層,滲透井中填滿滲透材料,使地面水與地下水層直接連結,產生快速滲透作用,將地面水儲存於地下水層,達到地下水位上升,防阻地層下陷,乾季又可適當抽取使用。 The technical structure of the groundwater level balance system is characterized in that the ground drilling permeate well at the surface water penetrates into the groundwater layer, and the permeation well is filled with the infiltration material, so that the surface water and the groundwater layer are directly connected, resulting in rapid infiltration and storage of the surface water. In the groundwater layer, the groundwater level rises, the anti-resistance stratum subsides, and the dry season can be appropriately extracted. 如申請專利範圍第1項所述地下水位平衡系統之技術結構,滲透井中裝入滲透管,縮短滲透距離,使大量地地面水,能更快速滲入地下水層儲存,使地下水位快速上升,防阻地層下陷。 For example, in the technical structure of the groundwater level balance system described in the first paragraph of the patent application, the permeation pipe is installed in the permeation well to shorten the penetration distance, so that a large amount of surface water can be infiltrated into the groundwater layer for storage, so that the groundwater level rises rapidly and the resistance is prevented. The formation subsided. 如申請專利範圍第1項所述地下水位平衡系統之技術結構之地面水,包括所有乾淨之水源,如屋頂之雨水。 For example, the surface water of the technical structure of the groundwater level balance system mentioned in the scope of patent application includes all clean water sources, such as rain on the roof. 如申請專利範圍第3項地下水位平衡系統之技術結構之地面水來源為屋頂之雨水時,直接與滲透管連結,大幅降低排水系統水量,防阻或降低都市水災發生,乾季時又方便取地下水使用、地下水污染監控、地下水汙染排除。 For example, when the surface water source of the technical structure of the groundwater level balance system of the third application is the rainwater of the roof, it is directly connected with the permeation pipe, which greatly reduces the water volume of the drainage system, prevents or reduces the occurrence of urban floods, and facilitates the groundwater in the dry season. Use, groundwater pollution monitoring, groundwater pollution exclusion.
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CN112666338A (en) * 2020-12-16 2021-04-16 杨玲 Fixed soil pollution real-time monitoring device

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CN112666338A (en) * 2020-12-16 2021-04-16 杨玲 Fixed soil pollution real-time monitoring device

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