TWI230783B - Method and system of average flowing velocity measurement in river - Google Patents
Method and system of average flowing velocity measurement in river Download PDFInfo
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- TWI230783B TWI230783B TW90112355A TW90112355A TWI230783B TW I230783 B TWI230783 B TW I230783B TW 90112355 A TW90112355 A TW 90112355A TW 90112355 A TW90112355 A TW 90112355A TW I230783 B TWI230783 B TW I230783B
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經濟部智慧財產局員工消費合作社印製 1230783 A7 一— B7____五、發明說明(1) 發明領域 本發明係關於一種測量河川水域平均流速之方法與系 統,尤其關於一種於挾帶泥沙的河川水域中測量平均流速 之方法與系統。 發明背景 台灣河川坡陡流急,水流觀測極其不易。每逢暴雨時 節水流湍急,河川流量漲退迅速,經常造成嚴重災害。本 省78%降雨集中於五至十月之颱風期間,洪水夾帶大量泥 沙,現場觀測困難重重,儀器極易流失損毀,人員安全更 是堪慮,使得河川流量測量倍增困難。但即使洪水期的高 速水流造成現場測量的困難度很高,流速等資料仍爲河川 整治與水資源工程規劃及設計之重要參考依據,因此仍須 設法取得。 應用聲波來探測水中物理特性本身即爲一門深入之學 問,其相關硏究相當多,例如應用聲波來探測海洋底部之 變動(Goff,1999;Paige,2000),以及在海下尋找某些魚群 或結構物(Volovov,1999)。目前最新之應用則是利用二維 海中聲波組來監測海中船隻(潛水艇)之移動(楊文彰, 1993 ;陳琪芳,1999)。然聲波一般均應用於海洋工程或海 洋探測,甚少用於河川。原因之一是,海中需求的是單點 流速或垂直流速剖面,因而目前一般商業上發展之流速測 量儀器均設計爲測量單點流速或垂向之流速。然而在河川 中,吾人所感興趣的卻是流量。因此在河川中,平均流速 4LIU/200101TW 1 裝--- (請先閱讀背面之注意事項再填寫本頁) · 訂L--- # 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) A7 1230783 B7 五、發明說明(丄) 係爲測量重點,而非單點流速。 (請先閱讀背面之注咅心事項再填寫本頁) 習知技術包括許多測單點流速之儀器,如SONTEK公 司推出的ARGONAUT-XR,其最大可測到6m/s之流速, 而 ADV ( Acoustic Doppler Velocimeter)可在 250 公尺內 測量到0.5m/s之流速。此外,該公司亦推出ADP( Acoustic Doppler Profiler ),其於海中可在500公尺內測量到10m/s 之流速。該公司更進一步將ADV與ADP結合爲PC-ADP (Pulse-Coherent Acoustic Doppler Profile),唯其只能觀 測到12公尺遠之距離,但解析度達1.6公分。其他公司亦 有類似之產品。 經濟部智慧財產局員工消費合作社印製 應用於河川中之最新流速測量方法爲利用都卜勒超聲 波儀來測量河川之垂直流速剖面(Lemmin & Rolland, 1997 ),這方面已經獲得了一定程度的成功。配合聲波探 測,Imran,Pafker & Pirmez於1999年提出聲波與流速、 流量關係之理論,而國內則有盧昭堯於1995年至1997年 間所提出的相關理論。上述測量方法係利用超聲波流速剖 面儀垂直解析之能力來測量河川中之速度剖面,再配合邱 式理論來求流量。然上述方法不僅有理論上及儀器架設上 的問題,最大的問題更在於無法克服河川中泥沙所產生的 影響。 另一套類似的儀器是由韓國昌民公司所推出的 SONIC FLOW。該儀器係利用超音波垂向射入水中,再利 用都卜勒效應測量河川垂向之平均流速。此儀器測速之最 大範圍爲3m/s,然其缺點之一亦爲無法使用於泥沙含量多 4LIU/200101TW 2 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) 經濟部智慧財產局員工消費合作社印製 1230783 A7 B7 五、發明說明(3 ) 之河川。另外,該儀器於使用上係設計爲手提式,因此適 用於小溪,但不適用於大河。 發明槪述 本發明係關於一種測量河川水域平均流速之方法與系 統,尤其關於一種於挾帶泥沙的河川水域中測量平均流速 之方法與系統。本發明以聲波發射器於待測河川水域之A 端發射一聲波,並以聲波接收器於B端接收該聲波;同時, 於B端亦發射一聲波,並於A端接收之。其中A、B兩端 係分別位於河川水域之上下游。記錄兩聲波於河川水域中 傳播之時間並求得一時間差,據以推斷出水流於A、B兩 端間之平均流速。將不同高程之流速予以積分,則得到河 川水域某斷面之流量。 本發明可包含一泥沙含量檢測器,以測得之泥沙含量 做爲選擇適當測量儀器之依據。本發明之聲波發射器及聲 波接收器可爲同一裝置(發射及接收雙用),以簡化儀器。 聲波發射器及聲波接收器亦可設置於一垂直槓上,以測量 河川水域之某斷面中,不同高程之流速。 圖式之簡單說明 圖1繪示本發明測量河川水域平均流速之方法流手呈 圖。 圖2爲本發明實施例之現場測量示意圖。 圖3爲本發明實施例之現場測量系統配置圖。 4LIU/200101TW 3 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) --—---- --------r 訂—ί------- (請先閱讀背面之注意事項再填寫本頁) 1230783 A7 B7 五、發明說明(+) 圖4爲本發明實施例之垂直槓示意圖。 圖式元件符號說明 經濟部智慧財產局員工消費合作社印製 A,A,,B,B,,Η 測量端 D 河道寬度 U! A、B兩端間之測量流速 u2 A’、B’兩端間之測量流速 a 川與U2之夾角 301, 301, 聲波產生器 302, 302’ 聲波發射器 303, 303’ 聲波接收器 304, 304’ 濾波器 305, 305’ 放大器 306 資料傳送組 307 微處理器 308 泥沙含量檢測器 309, 309’ 垂直槓 Z 1 5 Z2 5 .....? Z7 聲波發射器及接收器高程(z座標) Ul,u2,……,U7 不同高程之平均流速 (請先閱讀背面之注意事項再填寫本頁) 發明之詳細說明 圖1繪示本發明測量河川水域平均流速之方法流程 圖。 步驟101,首先測量待測河川水域中之泥沙含量及濃 4LIU/200101TW 4 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) 1230783Printed by the Consumer Cooperative of the Intellectual Property Bureau of the Ministry of Economic Affairs 1230783 A7 — B7____ V. Description of the Invention (1) Field of the Invention The present invention relates to a method and system for measuring the average flow velocity of river waters, especially to a river with mud and sand. Methods and systems for measuring average velocity in water. BACKGROUND OF THE INVENTION The river slopes in Taiwan are steep and the current is extremely difficult to observe. During heavy rains, the water flow is turbulent and river flows rise and fall rapidly, often causing severe disasters. 78% of the rainfall in the province was concentrated during the typhoon from May to October. Floods carried a large amount of sediment. Observations on the site were difficult, the instrument was easily lost and damaged, and personnel safety was a concern, making river flow measurement more difficult. However, even if the high-speed water flow during the flood period makes the on-site measurement difficult, data such as flow velocity are still important references for river improvement and water resource engineering planning and design, so it must be managed. The use of sound waves to detect the physical properties of water is an in-depth study, and there are many related studies, such as the use of sound waves to detect changes in the bottom of the ocean (Goff, 1999; Paige, 2000), and the search for certain fish schools or Structures (Volovov, 1999). The latest application is the use of two-dimensional underwater acoustic wave groups to monitor the movement of ships (submarines) in the sea (Yang Wenzhang, 1993; Chen Qifang, 1999). However, acoustic waves are generally used in marine engineering or ocean exploration, and rarely used in rivers. One of the reasons is that a single-point velocity or vertical velocity profile is required in the sea. Therefore, current commercial flow velocity measuring instruments are generally designed to measure single-point velocity or vertical velocity. In rivers, however, we are interested in flow. Therefore, in rivers, the average flow rate is 4LIU / 200101TW 1 pack --- (Please read the precautions on the back before filling this page) · Order L --- # This paper size applies to China National Standard (CNS) A4 specifications (210 X 297 mm) A7 1230783 B7 V. Description of the Invention (丄) It is the measurement focus, not the single-point velocity. (Please read the note on the back before filling this page.) Known technologies include many instruments that measure single-point flow velocity, such as the ARGONAUT-XR introduced by SONTEK, which can measure a maximum flow velocity of 6m / s, and ADV ( Acoustic Doppler Velocimeter) can measure a velocity of 0.5m / s within 250 meters. In addition, the company also launched ADP (Acoustic Doppler Profiler), which can measure a velocity of 10m / s in the sea within 500 meters. The company further combined ADV and ADP into a PC-ADP (Pulse-Coherent Acoustic Doppler Profile), which can only observe a distance of 12 meters, but the resolution is 1.6 cm. Other companies have similar products. The latest flow velocity measurement method applied to rivers printed by the Employees' Cooperatives of the Intellectual Property Bureau of the Ministry of Economic Affairs is the use of Doppler ultrasonics to measure the vertical velocity profile of rivers (Lemmin & Rolland, 1997). This has been achieved to a certain extent. success. In conjunction with sound wave detection, Imran, Pafker & Pirmez proposed the theory of the relationship between sound waves and flow velocity and flow rate in 1999, while in China there are related theories proposed by Lu Zhaoyao from 1995 to 1997. The above measurement method uses the vertical resolution of an ultrasonic velocity profiler to measure the velocity profile in a river, and then uses Qiu's theory to calculate the flow. However, the above method not only has problems in theory and erection of equipment, the biggest problem is that it cannot overcome the effects of sediment in rivers. Another similar instrument is the SONIC FLOW introduced by Korea Changmin. This instrument uses ultrasonic waves to shoot vertically into the water, and then uses the Doppler effect to measure the average vertical flow velocity of the river. The maximum speed range of this instrument is 3m / s, but one of its shortcomings is that it cannot be used for more sediment content 4LIU / 200101TW 2 This paper size is applicable to China National Standard (CNS) A4 (210 X 297 mm) Ministry of Economic Affairs Printed by the Intellectual Property Bureau Staff Consumer Cooperative 1230783 A7 B7 V. The River of Invention Description (3). In addition, the instrument is designed to be portable for use in the upper system, so it is suitable for small streams, but not for large rivers. Summary of the Invention The present invention relates to a method and system for measuring average flow velocity in river waters, and more particularly, to a method and system for measuring average flow velocity in river waters with mud and sand. In the present invention, a sound wave transmitter transmits a sound wave at the A terminal of the river water to be measured, and a sound wave receiver receives the sound wave at the B terminal; meanwhile, a sound wave is also transmitted at the B terminal, and is received at the A terminal. The two ends of A and B are located above and below the river waters. Record the time when two acoustic waves propagate in the river waters and find a time difference, so as to infer the average velocity of the water flow between the A and B ends. By integrating the velocity at different elevations, the flow in a section of the river waters can be obtained. The present invention may include a sediment content detector, and use the measured sediment content as a basis for selecting an appropriate measuring instrument. The acoustic wave transmitter and the acoustic wave receiver of the present invention can be the same device (dual-use for transmitting and receiving) to simplify the instrument. Acoustic transmitters and receivers can also be installed on a vertical bar to measure the velocity of flow at different elevations in a section of river waters. Brief Description of the Drawings Figure 1 shows the presenter's method for measuring the average velocity of river waters in the present invention. FIG. 2 is a schematic diagram of on-site measurement according to an embodiment of the present invention. FIG. 3 is a configuration diagram of a field measurement system according to an embodiment of the present invention. 4LIU / 200101TW 3 This paper size is applicable to China National Standard (CNS) A4 (210 X 297 mm) ------- -------- r Order—ί ------- ( (Please read the notes on the back before filling this page) 1230783 A7 B7 V. Description of the invention (+) Figure 4 is a schematic diagram of the vertical bar of the embodiment of the present invention. Symbols of graphic elements indicate the printing of A, A, B, B, B at the Consumer Property Cooperative of the Intellectual Property Bureau of the Ministry of Economics. Measured end D. Channel width U! Measured flow velocity u2 between both ends of A and B. A ', B' both ends. Measured flow rate a. The angle between Sichuan and U2 301, 301, sonic generator 302, 302 'sonic transmitter 303, 303' sonic receiver 304, 304 'filter 305, 305' amplifier 306 data transmission group 307 microprocessor 308 Sediment content detector 309, 309 'Vertical bar Z 1 5 Z2 5 .....? Z7 Acoustic transmitter and receiver elevation (z coordinate) Ul, u2, ..., U7 Average velocity of different elevations (please (Read the precautions on the back before filling this page) Detailed description of the invention Figure 1 shows the flow chart of the method for measuring the average flow velocity of river waters according to the present invention. Step 101: First measure the sediment content and concentration in the river water to be measured. 4LIU / 200101TW 4 This paper is in accordance with Chinese National Standard (CNS) A4 (210 X 297 mm) 1230783
經濟部智慧財產局員工消費合作社印製 五、發明說明(5) 度。一般河川水域中皆不免有泥沙的存在,爲了解決習知 技術的困難,本發明之測量河川水域平均流速方法包含一 泥沙含量檢測步驟。 待掌握待測河川水域之泥沙含量後,即進入步驟 102 ’依照泥沙含量及濃度選擇聲波發射/接收器。由於河 川水域中的泥沙會使聲波振幅減小,因此需配合泥沙濃度 選擇適當的儀器。 聲波在介質中傳遞時,是以壓力波的方式傳遞,而其 壓力隨距離之變化爲Printed by the Consumer Cooperatives of the Intellectual Property Bureau of the Ministry of Economic Affairs 5. Description of invention (5) Degree. In general, the presence of sediment is inevitable in river waters. In order to solve the difficulties of conventional techniques, the method for measuring the average flow velocity in river waters of the present invention includes a step of detecting sediment content. After grasping the sediment content in the river waters to be measured, it proceeds to step 102 ′ to select the sonic transmitter / receiver according to the sediment content and concentration. As the sediment in river water will reduce the acoustic wave amplitude, it is necessary to select an appropriate instrument in accordance with the sediment concentration. When a sound wave is transmitted in a medium, it is transmitted as a pressure wave, and the change of its pressure with distance is
Pr-Ps'f{r\e~ar ( 1) 其中6爲接收端之壓力振幅,爲發射端之壓力振 幅’ 爲聲波通過介質時之耗能,表示介質會吸收聲波之 能量,因此a爲介質之參數。/(r)爲聲波傳遞時之能量擴 散’可視爲幾何形狀的函數。例如在一三維無邊界之形狀 下,外)=士;而在一二維傳播之壓力場,外)=士; 一維 之傳播則視傳播渠道形狀而定。 聲波振幅的單位一般以分貝(dB)來計算。將(1) 式取201og1()得 20 log10 Pr = 20 log10 Ps + 20 log,〇 f(r) - 20ar log10 e ( 2 ) 一般麥克風是將聲壓轉換成電壓値輸出,因此(2)式 中之聲壓得以電壓來表示。而將電壓轉換爲聲壓之公式爲 (y \ 201〇g10|^^> ySPL^VL-SEN ( 3) 4LIU/200101TW 5 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) 裝--------^訂L------- (請先閱讀背面之注意事項再填寫本頁) A7 !23〇783 Β7 五、發明說明(k ) 在空氣中,=20< ;但在水中,々=1此。其中SPL (sound pressure level )是由聲波能量大小(voltage level, VL)減去儀器本身之靈敏度(SEN)而得,而聲波能量大 小VL係由下式計算 VL = 20lo^〇^/fref (4) 因爲SEN之參考電壓Vref爲IV,因此在第(4)式之 計算中亦採Vref = IV。第(4)式中之V即爲所發射或接 收之聲波電壓大小。SEN係爲儀器本身之靈敏度,SEN値 愈小,表示儀器之靈敏度愈高。而收發同體之水下麥克風, 其發射與接收之靈敏度亦不一定相同。 令 201og1()/(r) = //(r)且 a = 20alog1()e,可將第(2)式改寫 爲 VLr = VLS + SENr - SENs + H(r)-〇cr ( 5) α係爲一介質參數。此參數代表當聲波通過介質時, 於該介質中所消耗的能量;亦即,聲波通過含泥沙之水流 的能量消減率。α與泥沙濃度Μ以及聲波頻率f之關係爲 α = α(Μ,/),需由大量室內實驗來求得各種不同泥沙濃度及 聲波頻率下之α値。以本發明之一實施例而言,實驗結果 顯示濃度Μ及α値在聲波頻率5Κ且頻率固定下成近似線 性之關係。而在濃度固定下Μ,α値與聲波頻率也約呈線 性。 在決定α値之後,可根據所得之^値調整距離或選擇 適當之儀器。舉例來說,若以某麥克風發出10V大小之聲 4LIU/200101TW 〈 本紙張尺度適用中國國家標準(CNS)A4規格(21〇 X 297公爱) (請先閱讀背面之注意事項再填寫本頁) |裝--------訂----- 摹 經濟部智慧財產局員工消費合作社印製 經濟部智慧財產局員工消費合作社印製 1230783 A7 __ _____^^ B7 __ 五、發明說明(")) 波’並假設其發射聲波及接收聲波之靈敏度相同,均爲 _211.3dB,則聲波傳遞至接收端時之聲音大小依照(5)式 計算可得 KLr=20k)g(l0/1)+(_211.3)_(-211.3) +外)—欲。假設 待測河川水域爲一維聲場,y(r):=+,而河川水域中含有 微量泥沙(α = 0·01 ),則距離r公尺時,聲波大小爲 % =20-211·3 + 211·3 + (〇 —2〇1〇g严)一〇olr = 2〇- 101〇g卜001r。 當聲波由發射端傳遞1〇〇公尺時(r=100),接收端之聲波 大小爲-ldB。但聲波接收器實際上接收到的聲波大小需扣 除靈敏度’因此聲波接收器所接收到的聲波大小爲 -ldB-(-211.3dB)=21〇.3dB。若聲波接收器位於200公尺 外’則接收到之聲波大小爲206.3dB。 因此依照河川水域中之泥沙含量及濃度,可選擇具有 適當靈敏度的儀器做爲聲波發射器及聲波接收器。 選定聲波發射/接收器之後,進行步驟1〇3,由聲波 產生器形成具有適當頻率的聲波。由於適用於本發明之較 佳微波頻率係介於5〇〇Hz至1kHz之間,且針對不同測量 條件需要不同的入射波長與頻率,因此需經由聲波形產生 器來形成適當的聲波。 當具有適當頻率之聲波形成之後,即進入步驟104, 由A端發射上述適當頻率之聲波。本發明的實施例之一係 利用水下麥克風於河川水域之A端發射已選定頻率之聲 波’然而本發明並不限定以水下麥克風做爲發射聲波之裝 置’任何其他可用以發射聲波之設備皆爲本發明所意圖保 4LIU/200101TW 7 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) --------r ^ - L------- (請先閱讀背面之注意事項再填寫本頁) 1230783 經濟部智慧財產局員工消費合作社印製 A7 B7 五、發明說明(8 ) 護之範圍。 步驟105,於該河川水域之B端接收由a端傳來的該 聲波。同樣地,本發明的實施例之一係利用水下麥克風做 爲接收聲波之裝置,然而本發明並非僅限於使用水下麥克 風來接收聲波,任何其他可用以接收聲波之設備皆爲本發 明所意圖保護之範圍。 步驟106,記錄聲波由A端傳至B端所需之第一時間。 由於聲波傳遞之速度極快,時間記錄裝置之精度必須十分 準確。關於精度的要求將敘述如后。 於進行步驟104、步驟105、及步驟106的同時,亦可 一倂進行步驟104a、105a、及106a。步驟104a,於B端 亦發射一適當頻率之聲波。步驟105a,於A端接收由B 端傳來的該聲波。步驟106a,記錄聲波由B端傳至A端 所需之第二時間。同樣地,本發明的實施例之一係利用水 下麥克風做爲發射及接收聲波之裝置,然而本發明並非僅 限於使用水下麥克風來發射及接收聲波,任何其他可用以 發射及接收聲波之設備皆爲本發明所意圖保護之範圍。在 本發明之一具體實施例中,A、B兩端所發射之聲波係爲 同一頻率,且需同時發射(也就是步驟l〇4a、105a、及106a 與步驟104、105、及106需同步實施),以避免測量上的 誤差。 步驟107,由第一時間以及第二時間推算聲波於A、B 兩端傳遞之時間差△/,並據以計算A、B兩端間之平均流 速。當A、B兩端間某一高程之平均流速測量完畢後,進 4LIU/200101TW 〇 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) I I------I----------訂--_------- (請先閱讀背面之注意事項再填寫本頁) 1230783 A7 B7 五、發明說明(q ) 入步驟108,判斷是否已經測完A、B兩端間所有高程之 平均流速。由於河川水域斷面中不同高程通常會有流速的 差異,若尙未測量所有高程之平均流速,則進行步驟110, 選則令一高程並重複測量步驟;若已經測量完所有高程之 平均流速,則進行步驟109,依照測得之數據計算斷面流 量。 河川水域平均流速與流量之計算說明如后。 假設A端至B端之距離爲R,聲速爲C,而u爲聲波 傳遞路徑中,介質的平均流速。當u與C同向時(假設自 A端至B端爲順流),聲波於該介質中由A端傳遞至B端 所需的時間爲 (請先閱讀背面之注意事項再填寫本頁) •ΆΒPr-Ps'f {r \ e ~ ar (1) where 6 is the pressure amplitude at the receiving end and is the pressure amplitude at the transmitting end 'is the energy consumed by the sound wave as it passes through the medium, indicating that the medium will absorb the energy of the sound wave, so a is Parameters of the medium. / (r) is the energy diffusion 'when the sound wave is transmitted, which can be regarded as a function of the geometric shape. For example, in a three-dimensional shape with no boundaries, outer) = Shi; and in a two-dimensional propagation pressure field, outer) = Shi; one-dimensional propagation depends on the shape of the propagation channel. The unit of sound wave amplitude is generally calculated in decibels (dB). The formula (1) is 201og1 () to obtain 20 log10 Pr = 20 log10 Ps + 20 log, 〇f (r)-20ar log10 e (2) The general microphone converts sound pressure into voltage 値 output, so formula (2) The sound pressure in medium is expressed by voltage. The formula for converting voltage to sound pressure is (y \ 201〇g10 | ^^ > ySPL ^ VL-SEN (3) 4LIU / 200101TW 5 This paper size is applicable to China National Standard (CNS) A4 (210 X 297 cm) (Li) Install -------- ^ Order L ------- (Please read the precautions on the back before filling out this page) A7! 23〇783 Β7 5. Description of the invention (k) in the air , = 20 <; But in water, 々 = 1 this. Among them, SPL (sound pressure level) is obtained by subtracting the sensitivity (SEN) of the instrument itself from the voltage level (VL), and the acoustic energy level VL is Calculate VL = 20lo ^ 〇 ^ / fref from the following formula (4) Because the reference voltage Vref of SEN is IV, Vref = IV is also used in the calculation of formula (4). V in formula (4) is The transmitted or received sound wave voltage. SEN is the sensitivity of the instrument itself. The smaller the SEN 値, the higher the sensitivity of the instrument. The sensitivity of the transmitting and receiving underwater microphones is not necessarily the same. 201og1 () / (r) = // (r) and a = 20alog1 () e, the equation (2) can be rewritten as VLr = VLS + SENr-SENs + H (r) -〇cr (5) α system Is a medium parameter. The parameter represents the energy consumed in the medium when the sound wave passes through the medium; that is, the energy reduction rate of the sound wave through the water flow containing sediment. The relationship between α and the concentration of sediment M and the frequency of sound wave f is α = α (Μ , /), Α 値 at various sediment concentrations and acoustic frequencies needs to be obtained through a large number of indoor experiments. According to an embodiment of the present invention, the experimental results show that the concentrations M and α 値 are at a sound frequency of 5K and the frequency is fixed. The relationship becomes approximately linear. At a fixed concentration M, α 値 and the frequency of the sound wave are also approximately linear. After determining α 値, you can adjust the distance or choose an appropriate instrument based on the obtained 値 値. A microphone emits a 10V sound 4LIU / 200101TW 〈This paper size is applicable to China National Standard (CNS) A4 (21〇X 297 public love) (Please read the precautions on the back before filling this page) | Installation ---- ---- Order ----- 印 Printed by the Consumer Cooperatives of the Intellectual Property Bureau of the Ministry of Economic Affairs Printed by the Consumer Cooperatives of the Intellectual Property Bureau of the Ministry of Economic Affairs Printed by 1230783 A7 __ _____ ^^ B7 __ 5. Explanation of the Invention (")) Wave ' And assume its emission The sensitivity of the wave and the received sound wave are the same, both are _211.3dB. Then the sound size when the sound wave is transmitted to the receiving end is calculated according to formula (5). KLr = 20k) g (l0 / 1) + (_ 211.3) _ (- 211.3) + outside)-desire. Assume that the river water to be measured is a one-dimensional sound field, y (r): = +, and the river water contains trace sediment (α = 0 · 01). When the distance is r meters, the sound wave size is% = 20-211 · 3 + 211 · 3 + (0-2010 g) 100olr = 20-101 g g 001r. When the sound wave is transmitted by 100 meters from the transmitting end (r = 100), the size of the sound wave at the receiving end is -ldB. But the size of the sound wave actually received by the sound wave receiver needs to be deducted from the sensitivity ’, so the size of the sound wave received by the sound wave receiver is -ldB-(-211.3dB) = 20.3dB. If the sound wave receiver is located 200 meters away, the size of the received sound wave is 206.3dB. Therefore, according to the sediment content and concentration in river waters, instruments with appropriate sensitivity can be selected as the acoustic wave transmitter and acoustic wave receiver. After the sound wave transmitter / receiver is selected, step 103 is performed, and a sound wave having an appropriate frequency is formed by the sound wave generator. Since the preferred microwave frequency suitable for the present invention is between 500 Hz and 1 kHz, and different incident wavelengths and frequencies are required for different measurement conditions, a sound waveform generator is required to form a suitable sound wave. When a sound wave with an appropriate frequency is formed, the process proceeds to step 104, and the above-mentioned sound wave with an appropriate frequency is emitted from the A terminal. One of the embodiments of the present invention is the use of an underwater microphone to emit a sound wave of a selected frequency at the A end of river waters. However, the present invention is not limited to using an underwater microphone as a device for transmitting sound waves. Any other device that can be used to emit sound waves It is the intention of the present invention to guarantee 4LIU / 200101TW 7 This paper size is applicable to China National Standard (CNS) A4 (210 X 297 mm) -------- r ^-L ------- ( (Please read the notes on the back before filling this page) 1230783 Printed by the Consumer Cooperatives of the Intellectual Property Bureau of the Ministry of Economic Affairs A7 B7 V. Description of the invention (8). Step 105: Receive the sound wave from the a terminal at the B terminal of the river water. Similarly, one of the embodiments of the present invention uses an underwater microphone as a device for receiving sound waves. However, the present invention is not limited to using an underwater microphone to receive sound waves. Any other device capable of receiving sound waves is intended by the present invention. The scope of protection. Step 106: Record the first time required for the sound wave to pass from the A terminal to the B terminal. Because the speed of sound wave transmission is extremely fast, the accuracy of the time recording device must be very accurate. The accuracy requirements will be described later. While performing steps 104, 105, and 106, steps 104a, 105a, and 106a can also be performed at once. In step 104a, a sound wave of an appropriate frequency is also transmitted at the B terminal. In step 105a, the sound wave from the B terminal is received at the A terminal. In step 106a, the second time required for the sound wave to travel from the B terminal to the A terminal is recorded. Similarly, one of the embodiments of the present invention uses an underwater microphone as a device for transmitting and receiving sound waves. However, the present invention is not limited to using an underwater microphone to transmit and receive sound waves. Any other device that can be used to transmit and receive sound waves All are within the scope of the present invention. In a specific embodiment of the present invention, the sound waves transmitted at both ends of A and B are of the same frequency and need to be transmitted simultaneously (that is, steps 104a, 105a, and 106a and steps 104, 105, and 106 need to be synchronized). Implementation) to avoid measurement errors. In step 107, the time difference Δ / transmitted by the sound waves at both ends of A and B is calculated from the first time and the second time, and the average flow velocity between the two ends of A and B is calculated based on it. After the measurement of the average flow velocity at a certain elevation between the two ends of A and B, enter 4LIU / 200101TW 〇 This paper size applies the Chinese National Standard (CNS) A4 specification (210 X 297 mm) I I ------ I ---------- Order --_------- (Please read the notes on the back before filling this page) 1230783 A7 B7 V. Description of the invention (q) Go to step 108 to determine whether The average velocity of all elevations between the two ends of A and B has been measured. Because different elevations in river water sections usually have velocity differences, if the average velocity of all elevations has not been measured, proceed to step 110, select one elevation and repeat the measurement steps; if the average velocity of all elevations has been measured, Then, step 109 is performed to calculate the cross-section flow according to the measured data. The calculation and explanation of the average velocity and discharge of river waters are as follows. Assume that the distance from the A end to the B end is R, the sound velocity is C, and u is the average flow velocity of the medium in the acoustic wave transmission path. When u and C are in the same direction (assuming that the current flows from end A to end B), the time required for sound waves to pass from end A to end B in the medium is (please read the precautions on the back before filling this page) • ΆΒ
R (6) 而當聲波由B端傳至A端時(逆流),所需的時間爲R (6) and when the sound wave passes from B to A (counter current), the time required is
^BA^ BA
R C — u (7) 由(6)、(7)可得兩時間差之一半爲R C — u (7) From (6) and (7) one half of the time difference is
AtAt
^AB —玄BA _ RU 〜RU 1 Η--r C2 \ ) (8) 經濟部智慧財產局員工消費合作社印製 2 C2-厂 C2 由於一般河川水域水流最快不超過l〇m/S,聲波在水 中之速度約爲1500m/s,因此^ AB —Xuan BA _ RU ~ RU 1 Η--r C2 \) (8) Printed by the Consumer Cooperatives of the Intellectual Property Bureau of the Ministry of Economic Affairs 2 C2-Plant C2 Because the general river water flow is no faster than 10m / S, The speed of sound waves in water is about 1500m / s, so
C 4·4χ1(Γ5。在一般工程 科學中,這個數字是可忽略的誤差。因此,利用聲波在順 流與逆流中傳遞時間不同的特性,可得到C 4 · 4χ1 (Γ5. In general engineering science, this number is a negligible error. Therefore, using the characteristics of the acoustic wave in the time difference between the forward and reverse current, we can get
4LIU/200101TW 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) 1230783 a7 B7 經濟部智慧財產局員工消費合作社印製 五、發明說明(L。) 其中,Δ/爲來回訊號接收時間之半,w爲聲波傳遞路 徑中介質流動之平均速度,而R爲發射端至接收端間之直 線距離。 一般待測河川水域之最大寬度可到500公尺(河口 處),最小也有1〇公尺(灌溉渠道);就灌溉渠道而言,待 測之流速最大可到lOm/sec。以灌溉渠道爲例,將寬度與 流速帶入第(9)式,可得= 0.0022秒。一般記錄器之精 度可達ΚΓ4秒,因此在[與R很大的情況下,使用一般儀器 測量不會有問題。但當w與R很小的時候,&的計算就會 有困難。爲了解決上述困難,本發明之較佳具體實施例以 下列方式架設於待測河川水域之兩岸。圖2爲本發明具體 實施例之現場測量示意圖。由(9)式可得知,當流速不變 時,A、B兩端距離愈遠,Δ/的値愈大,在固定信號截取 時間間距下所造成的誤差愈小。因此如圖2所示,本發明 實施例以非與流速平行的方式架設兩組儀器,但避免與流 速方向成90度角。圖2中之A、B兩端爲一組發射/接收 組,而A’、B’兩端爲另一組發射/接收組,其中兩組儀器 連線的夾角爲α,而待測河川水域兩岸間之寬度爲D。測 量時,每一組各會在測線方向得到平均流速( A、Β方 向)及U2 (A’、B’方向),而U!及U2之合速度大小爲 iRAsina。但此速度不一定平行於兩岸,爲了計算流量, 4LIU/200101TW 10 (請先閱讀背面之注意事項再填寫本頁) -裝--------^訂·!.-- #· 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) 1230783 A7 B7 五、發明說明((υ (請先閱讀背面之注意事項再填寫本頁) 可以控制體積(control volume )之觀念來檢查圖2中之三 角形Α’ΒΉ。因爲岸邊不會有出流量,因此A’B’斷面之垂 直流量即爲河川水域中任一斷面(如B’H)之流量。而垂 直A’B’斷面之速度分量爲UlSina,因此將UlSina對A’B’ 斷面積分即可得河川水域之流量。本實施例之好處爲測量 端可由硏究者自行選擇,而不需垂直於該河川水域之兩 岸,從而避免定垂線之誤差。 本發明之另一實施例亦可採用一組儀器來測量流量。 河川水域斷面之流量在曲線座標上可表示爲 Q=[u-dA (10) 其中J爲垂直流速之斷面面積。一般在實測時,都因 爲計算流量所需流速爲平行兩岸之方向,因此J之方向也 可以用兩岸平均切線方向來計算,而在水流動方向爲直線 之部份(一般是以河道中點之連線來考量),上式就可以不 用向量且採卡式座標寫成 Q = Wdydz 其中Y爲河川水域寬度方向,Z爲水深方向。若沿流 向方向(X方向)流量變化不大,Q可以寫成 經濟部智慧財產局員工消費合作社印製 Q = \V(iiudzdy)dx Ο。 L 2 其中I爲受測量河川水域區域長,π爲河川水域寬,A 爲水深,而W爲X方向之流速。 本發明實施例之測量因爲一定要與主流速方向成一夾 角,因此將原來(x,y,z)座標改爲(χ/Α,ζ)座標,X;爲 4LIU/200101TW 11 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) 12307^3 A7 B7 五、 原來之X軸,h爲將原來與;c軸垂直之 軸逆時鐘旋轉一 個0角。本發明實施例之測量是在新座標下做yi方向之積 分得一新流量Q’ Q’=\t%:Jh\dz(Kdyjhxdx' (12) 其中/2/,/^爲自(X,y)座標轉成(心力)座標之轉換 係數,/^=7/〇以夕,夕。夕爲測量線與流速方向之夾 角。若在(X,J〇座標上之流速爲(W,v),在新座標上之流 速爲(M/,V/ ),其間之關係爲4LIU / 200101TW This paper size is applicable to Chinese National Standard (CNS) A4 (210 X 297 mm) 1230783 a7 B7 Printed by the Consumer Cooperatives of the Intellectual Property Bureau of the Ministry of Economic Affairs 5. Description of the invention (L.) Among them, Δ / is a return signal At half of the receiving time, w is the average velocity of the medium flowing in the acoustic wave transmission path, and R is the linear distance from the transmitting end to the receiving end. Generally, the maximum width of the river water to be measured can reach 500 meters (at the estuary), and the smallest can also be 10 meters (irrigation channel). For the irrigation channel, the maximum flow velocity to be measured can reach 10 m / sec. Taking the irrigation channel as an example, the width and velocity are brought into equation (9), and we get = 0.0022 seconds. The accuracy of the general recorder can reach κΓ4 seconds, so in the case of [and R is very large, there is no problem in measuring with general instruments. But when w and R are small, the calculation of & will be difficult. In order to solve the above-mentioned difficulties, a preferred embodiment of the present invention is erected on both banks of the river water to be measured in the following manner. Fig. 2 is a schematic diagram of on-site measurement of a specific embodiment of the present invention. It can be known from equation (9) that when the flow velocity is constant, the farther the distance between the two ends of A and B is, the larger the 値 // is, and the smaller the error caused by the fixed signal interception time interval is. Therefore, as shown in Fig. 2, the embodiment of the present invention sets up two sets of instruments in a manner not parallel to the flow velocity, but avoids forming an angle of 90 degrees with the flow velocity direction. In Figure 2, the two ends of A and B are a transmitting / receiving group, and the two ends of A 'and B' are another transmitting / receiving group. The angle between the two groups of instruments is α, and the river waters to be measured The width between the two banks is D. During the measurement, each group will obtain the average velocity (A, B direction) and U2 (A ', B' direction) in the direction of the measurement line, and the combined velocity of U! And U2 is iRAsina. But this speed is not necessarily parallel to the two sides. In order to calculate the flow, 4LIU / 200101TW 10 (Please read the precautions on the back before filling this page) -Install -------- ^ Order ·! .-- # · 本Paper size applies Chinese National Standard (CNS) A4 (210 X 297 mm) 1230783 A7 B7 V. Description of invention ((υ (Please read the precautions on the back before filling this page) The concept of control volume can be controlled Check the triangle A′ΒΉ in Figure 2. Because there will be no outflow from the shore, the vertical flow of the A'B 'section is the flow of any section (such as B'H) in the river water. And the vertical The velocity component of the A'B 'section is UlSina, so the flow of river waters can be obtained by dividing UlSina with the A'B' section area. The advantage of this embodiment is that the measuring end can be selected by the researcher himself, without vertical It is located on both sides of the river water, so as to avoid the error of the vertical line. Another embodiment of the present invention can also use a set of instruments to measure the flow. The flow of the cross section of the river water can be expressed as the curve coordinate Q = [u-dA (10) where J is the cross-sectional area of vertical flow velocity. Generally measured At this time, because the flow velocity required to calculate the flow is parallel to the two banks, the direction of J can also be calculated by the average tangent direction of the two banks, and in the direction of the water flow is a straight line (usually the line connecting the midpoint of the river channel) (Consideration), the above formula can be used without vectors and the card-type coordinates can be written as Q = Wdydz where Y is the width of the river waters and Z is the depth of the water. If there is little change in the flow direction (X direction), Q can be written as the wisdom of the Ministry of Economy Printed by the Consumer Cooperative of the Property Bureau Q = \ V (iiudzdy) dx Ο. L 2 where I is the length of the river water area to be measured, π is the width of the river water area, A is the water depth, and W is the flow velocity in the X direction. Because the measurement must be at an angle with the main flow direction, the original (x, y, z) coordinates were changed to (χ / Α, ζ) coordinates, X; 4LIU / 200101TW 11 This paper scale applies Chinese national standards ( CNS) A4 specification (210 X 297 mm) 12307 ^ 3 A7 B7 V. The original X axis, h is the axis perpendicular to the original axis; c is rotated by a 0 angle counterclockwise. The measurement of the embodiment of the present invention is in the new Integrate in the yi direction under the coordinates Get a new flow Q 'Q' = \ t%: Jh \ dz (Kdyjhxdx '(12) where / 2 /, / ^ is the conversion coefficient from (X, y) coordinates to (heart force) coordinates, / ^ = 7 / 〇 is the evening, evening. The evening is the angle between the measurement line and the direction of the flow velocity. If the flow velocity at the (X, Jo) coordinate is (W, v), the flow velocity at the new coordinate is (M /, V /) , The relationship between
{W/=W V]=ucos θ - vsin θ ( 13 ) 測量之流速實際上爲v7,執行對V/之積分((12)式) 可得Q’爲 1 PCQ+L ^-\ζχιΘ Λ β = — I 丄u cos ^ - v sin 6dzdyx dxx (請先閱讀背面之注意事項再填寫本頁) 一裝 訂 # 經濟部智慧財產局員工消費合作社印製{W / = WV] = ucos θ-vsin θ (13) The measured flow velocity is actually v7, and the integral of V / is performed (formula (12)). Q 'is 1 PCQ + L ^-\ ζχιΘ Λ β = — I 丄 u cos ^-v sin 6dzdyx dxx (Please read the precautions on the back before filling out this page) One binding # Printed by the Ministry of Economic Affairs Intellectual Property Bureau Staff Consumer Cooperative
Qf= sinO— £0+I ih^vdydzdx-cos6— [[+L £ ^udydzdx L办 飞 L ϋ 1 =-Qsin Θ (14) 因爲v對j;之積分爲零,同時與(11)式比較後可知, 斜向測得之流量値與真實流量間之關係爲 Q'- - Qcos ΘQf = sinO— £ 0 + I ih ^ vdydzdx-cos6— [[+ L £ ^ udydzdx L L to fly L ϋ 1 = -Qsin Θ (14) because v is equal to j; the integral is zero and at the same time as (11) After comparison, the relationship between the obliquely measured flow rate 値 and the actual flow rate is Q'--Qcos Θ
因此單一組儀器仍然可以得到河川水域之流量値,但 4LIU/200101TW 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) 12 經濟部智慧財產局員工消費合作社印製 1230783 A7 _ — ____ B7 五、發明說明 是此時測線與河川水域流速間之夾角必須另外設法測量。 本實施例在規則渠道之誤差較小。 圖3爲本發明實施例之現場測裊系統配置圖。 本發明測量河川水域平均流速之系統包含聲波產生器 301及301’。由於適用於本發明之較佳微波頻率係介於 500Hz至1kHz之間,且針對不同測量條件需要不同的入 射波長與頻率,因此需經由聲波形產生器301及301,來开多 成適當的聲波。本發明並不限定包含兩個聲波發射器3〇1 及30Γ,亦可採用一個聲波發射器301與a、B兩端之聲 波發射器302及302’分別連接。 聲波產生器301及301’分別與聲波發射器302及302, 連接,以將適當波形之聲波由A端發射至B端。本發明的 實施例之一係利用水下麥克風做爲發射聲波之裝置,然而 本發明並非僅限於使用水下麥克風來發射聲波,任何其他 可用以發射聲波之設備皆爲本發明所意圖保護之範圍。另 外,在本發明之一具體實施例中,聲波發射器302及302’ 係在A、B兩端於同一時間發射同一頻率之聲波,以避免 測量上的誤差。 本發明之系統另包含聲波接收器303及303’,分別接 收由聲波發射器302及302’所發射之聲波。同樣地,本發 明的實施例之一係利用水下麥克風做爲接收聲波之裝置, 然而本發明並非僅限於使用水下麥克風來接收聲波,任何 其他可用以接收聲波之設備皆爲本發明所意圖保護之範 4LIU/200101TW 13 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公爱) ---^--------L------- (請先閱讀背面之注意事項再填寫本頁) 經濟部智慧財產局員工消費合作社印製 1230783 A7 B7 五、發明說明(丨+) 需注意的是’爲求測量之精確性,本發明之聲波發射 器302與聲波接收器303可爲同一裝置;而聲波發射器3〇2, 與聲波接收器303’亦可爲同一裝置。亦即,本發明之聲波 發射器302與聲波接收器303可爲一收發同體之聲波發射 /接收裝置;而聲波發射器302’與聲波接收器3〇3,亦可爲 一收發同體之聲波發射/接收裝置,以避免儀器之架設造 成聲波傳遞距離的誤差,並達到精簡儀器的目的。 本發明系統另可包含濾波器304及304,分別與聲波接 收器303及303’連接。濾波器304及304,係用以過濾聲波 接收器303及303’所接收的聲波,去除聲波中的雜訊。 本發明系統另可包含放大器305及305’分別與濾波器 304及304’連接。放大器305及305’係用以將濾波器304 及304’過濾後之聲波予以放大,以便於系統之測量與判斷。 本發明之系統包含一資料傳送組306,與聲波接收器 303及303’連接。資料傳送組306將聲波於該河川水域中 傳遞的時間資料以無線方式傳送至一遠端的工作站,以利 遠端之硏究者進行硏究。 本發明系統另包含一微處理器307,與資料傳送組306 連接。微處理器307係負責接收資料傳送組306傳送之聲 波傳遞時間資料,並針對聲波傳遞之時間資料進行待測河 川水域流速的運算。 本發明系統另包含一泥沙含量檢測器308,與資料傳 送組306連接。泥沙含量檢測器308檢測待測河川水域中 之泥沙濃度後,將檢測資料經由資料傳送組306傳送給遠 4LIU/200101TW 14 本紙張尺度適用中國國家標準(CNS)A4規格(210 X 297公釐) ·裝--------^訂 L--- (請先閱讀背面之注意事項再填寫本頁) # 1230783 A7Therefore, a single group of instruments can still get the flow of river water. However, the paper size of 4LIU / 200101TW is applicable to the Chinese National Standard (CNS) A4 specification (210 X 297 mm). 12 Printed by the Consumer Cooperative of Intellectual Property Bureau of the Ministry of Economic Affairs 1230783 A7 _ — ____ B7 V. The description of the invention is that the angle between the survey line and the velocity of the river water must be measured separately. The error in the regular channel is small in this embodiment. FIG. 3 is a configuration diagram of a field measurement system according to an embodiment of the present invention. The system for measuring the average flow velocity in river waters of the present invention includes sonic generators 301 and 301 '. Since the preferred microwave frequency suitable for the present invention is between 500 Hz and 1 kHz, and different incident wavelengths and frequencies are required for different measurement conditions, it is necessary to use the acoustic waveform generators 301 and 301 to drive into appropriate sound waves. . The present invention is not limited to including two acoustic wave transmitters 301 and 30Γ, and one acoustic wave transmitter 301 can be connected to the acoustic wave transmitters 302 and 302 'at both ends of a and B, respectively. The sound wave generators 301 and 301 'are connected to the sound wave transmitters 302 and 302, respectively, so as to transmit sound waves of appropriate waveforms from the A terminal to the B terminal. One of the embodiments of the present invention uses an underwater microphone as a device for transmitting sound waves. However, the present invention is not limited to using an underwater microphone to transmit sound waves. Any other device that can be used to transmit sound waves is within the scope of the present invention. . In addition, in a specific embodiment of the present invention, the sound wave transmitters 302 and 302 'transmit sound waves of the same frequency at the same time at both ends of A and B to avoid measurement errors. The system of the present invention further includes sound wave receivers 303 and 303 ', which respectively receive sound waves transmitted by the sound wave transmitters 302 and 302'. Similarly, one of the embodiments of the present invention uses an underwater microphone as a device for receiving sound waves. However, the present invention is not limited to using an underwater microphone to receive sound waves. Any other device that can receive sound waves is intended by the present invention. The norm of protection 4LIU / 200101TW 13 This paper size applies to China National Standard (CNS) A4 (210 X 297 public love) --- ^ -------- L ------- (Please read first Note on the back, please fill in this page again) Printed by the Consumer Cooperatives of the Intellectual Property Bureau of the Ministry of Economic Affairs 1230783 A7 B7 V. Description of the invention (丨 +) It should be noted that 'for the accuracy of the measurement, the acoustic wave transmitter 302 of the invention The acoustic wave receiver 303 may be the same device; and the acoustic wave transmitter 302 and the acoustic wave receiver 303 ′ may also be the same device. That is, the sound wave transmitter 302 and the sound wave receiver 303 of the present invention can be a sound wave transmitting / receiving device of the same body; and the sound wave transmitter 302 'and the sound wave receiver 303 can also be a body of a transmitting and receiving body. Acoustic wave transmitting / receiving device, in order to avoid the error of acoustic wave transmission distance caused by the installation of the instrument, and achieve the purpose of streamlining the instrument. The system of the present invention may further include filters 304 and 304, which are connected to the acoustic receivers 303 and 303 ', respectively. The filters 304 and 304 are used to filter the sound waves received by the sound wave receivers 303 and 303 'to remove noise in the sound waves. The system of the present invention may further include amplifiers 305 and 305 'connected to filters 304 and 304', respectively. The amplifiers 305 and 305 'are used to amplify the sound waves filtered by the filters 304 and 304' to facilitate the measurement and judgment of the system. The system of the present invention includes a data transmission group 306 connected to the acoustic receivers 303 and 303 '. The data transmission group 306 wirelessly transmits the time data transmitted by the sound waves in the river waters to a remote workstation for the researchers at the remote site to conduct research. The system of the present invention further includes a microprocessor 307 connected to the data transmission group 306. The microprocessor 307 is responsible for receiving the acoustic wave transmission time data transmitted by the data transmission group 306, and performing the calculation of the flow velocity of the river water to be measured based on the acoustic wave transmission time data. The system of the present invention further includes a sediment content detector 308, which is connected to the data transmission group 306. The sediment content detector 308 detects the sediment concentration in the river water to be measured, and transmits the detection data to the Yuan 4LIU / 200101TW via the data transmission group 306. 14 This paper size applies the Chinese National Standard (CNS) A4 specification (210 X 297). Li) · Install -------- ^ Order L --- (Please read the precautions on the back before filling this page) # 1230783 A7
B7 五、發明說明(\5 ) 端之硏究者,以做爲選擇聲波發射/接收器302、302’、 303、303’之依據。 圖4爲本發明實施例之垂直槓示意圖。由於河川水域 之流速會依照水深不同而有些許改變,時最好能夠測量各 不同水深之流速,以確保測量的准確性。如圖4,聲波發 射器302及302’與聲波接收器303及303’係以可滑動的方 式設置於垂直槓309及309’上,其中聲波發射器302及302, 與聲波接收器303及303’之高程(z座標)係由機械或人 工控制。當聲波發射器302及302’與聲波接收器303及303, 均位於ζ:處時,測得之流速爲^ ;位於Z2處時,測得之流 速爲ί ;以此類推。測得不同高程之平均流速之後,將其 積分,即得斷面流量2 Z itli 〇 需注意的是,本發明本發明並非僅限定於測量河川之 平均流速,亦可應用於湖泊、水庫、池塘等水域之平均流 速測量。 以上較佳具體實施例之詳述係用以更加淸楚地描述本 發明之特徵與精神,而非用以限制本發明之範疇。本發明 之申請專利範圍的範疇應該根據上述的說明作最寬廣的解 釋,並涵蓋所有可能均等的改變以及具均等性的安排。B7 V. Researchers of the invention description (\ 5) regard it as the basis for selecting the sound wave transmitter / receivers 302, 302 ', 303, 303'. FIG. 4 is a schematic diagram of a vertical bar according to an embodiment of the present invention. Since the flow velocity of river waters varies slightly according to the water depth, it is best to measure the flow velocity at different water depths to ensure the accuracy of the measurement. As shown in FIG. 4, the sound wave transmitters 302 and 302 ′ and the sound wave receivers 303 and 303 ′ are slidably arranged on the vertical bars 309 and 309 ′, among which the sound wave transmitters 302 and 302 and the sound wave receivers 303 and 303 The elevation (z coordinate) is controlled mechanically or manually. When the sound wave transmitters 302 and 302 ′ and the sound wave receivers 303 and 303 are both located at ζ :, the measured flow velocity is ^; when they are located at Z2, the measured flow velocity is ί; and so on. After measuring the average flow velocity at different elevations, integrate it to obtain the cross-sectional flow rate 2 Z itli. It should be noted that the present invention is not limited to measuring the average flow velocity of rivers, but can also be applied to lakes, reservoirs, and ponds. Measurement of the average flow velocity in other waters. The above detailed description of the preferred embodiments is used to more clearly describe the features and spirit of the present invention, but not to limit the scope of the present invention. The scope of the patentable scope of the present invention should be explained in the broadest sense according to the above description, and cover all possible equal changes and arrangements with equality.
4LIU/200101TW 15 本紙張尺度適用中國國豕標準(CNS)A4規格(21〇 X 297公着) ·裝--------^訂L------- Γ讀先閱讀背面之注意事項再填寫本頁) 經濟部智慧財產局員工消費合作社印製4LIU / 200101TW 15 This paper size is applicable to China National Standard (CNS) A4 specification (21〇X 297) · Install -------- ^ Order L ------- Γ Read first read the back (Please note this page before completing this page) Printed by the Consumer Cooperatives of the Intellectual Property Bureau of the Ministry of Economic Affairs
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TWI465721B (en) * | 2013-01-16 | 2014-12-21 | Univ Ishou | A method for surface velocity estimation of river water |
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TWI465721B (en) * | 2013-01-16 | 2014-12-21 | Univ Ishou | A method for surface velocity estimation of river water |
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