TWI650574B - Tdr device and method for monitoring subsidence variation - Google Patents

Tdr device and method for monitoring subsidence variation Download PDF

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TWI650574B
TWI650574B TW107106532A TW107106532A TWI650574B TW I650574 B TWI650574 B TW I650574B TW 107106532 A TW107106532 A TW 107106532A TW 107106532 A TW107106532 A TW 107106532A TW I650574 B TWI650574 B TW I650574B
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subsidence
waveform
band
time domain
sinking
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TW107106532A
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TW201937195A (en
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鐘志忠
簡煒烽
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國立中央大學
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Abstract

本發明係一種時域反射式監測沉陷變化裝置及其方法,包括一時域反射式感測裝置裝設在一待測環境中,以擷取一量測波形。一資料處理器比對量測波形之一量測基準波段,與一參考波形之一參考基準波段比對,以取得一誤差值,並比對量測波形之一量測沉陷波段以及參考波形之一參考沉陷波段,產生一沉陷差值,最後根據誤差值及沉陷差值之差異量,產生形成一波形時間差值,並帶入一實際沉陷量方程式取得一實際沉陷量。本發明利用時域反射可用於多個深度,且自動化偵測沉陷量,並可濾除系統中所產生的誤差值,以達到精確數值量測。The invention relates to a time domain reflection type monitoring subsidence changing device and a method thereof, which comprise a time domain reflective sensing device installed in an environment to be tested to extract a measuring waveform. A data processor compares the reference band with one of the measured waveforms, and compares with one of the reference waveforms to obtain an error value, and compares the sinking band and the reference waveform with one of the measured waveforms. A reference sinking band is used to generate a sinking difference. Finally, according to the difference between the error value and the sinking difference, a waveform time difference is generated, and an actual sinking amount equation is taken to obtain an actual sinking amount. The present invention utilizes time domain reflection for multiple depths, and automatically detects the amount of sinking, and can filter out error values generated in the system to achieve accurate numerical measurements.

Description

時域反射式監測沉陷變化裝置及其方法Time domain reflective monitoring subsidence changing device and method thereof

本發明係有關一種測量地層沉陷量之技術,特別是指一種時域反射式監測沉陷變化裝置及其方法。The present invention relates to a technique for measuring formation subsidence, and more particularly to a time domain reflective monitoring subsidence changing device and method therefor.

隨著水資源需求的增加,河川以及水庫中的水已供不應求,導致人們開始抽取地下水以彌補水資源的不足,導致超抽地下水的情形日益嚴重,不斷超抽地下水的結果造成地下水鹽化、土壤鹽化以及地層下陷等影響,因此如何有效監控土壤沉陷量變化,以預防土壤下陷,以及保護環境,儼然已成為一個相當重要的課題。As the demand for water resources increases, the water in rivers and reservoirs is in short supply, leading people to start pumping groundwater to make up for the shortage of water resources. As a result, the situation of over-pumping groundwater is becoming more and more serious. The result of continuous pumping of groundwater causes groundwater salinization and soil. Salinization and subsidence of the formation, so how to effectively monitor changes in soil subsidence to prevent soil subsidence and protect the environment has become a very important issue.

目前傳統量測下陷的方法,係於地表面定期實施大面積或局部性之水準測量,以掌握地形地物地貌之變化。在量測沉陷量時,需設置適量之基準點,並由各基準點的地層下陷量,可繪出下陷量等高線,以求出下陷中心,並經由多次不同時間之測量結果比較,求出地層隨時間之下陷量。但是此種方法相當耗費人力以及時間,且測量之時間間隔較大,平均二至三月才能量側一次,較不易獲得連續之地層下陷資料。At present, the traditional method of measuring subsidence is to carry out large-scale or local leveling on the ground surface regularly to grasp the changes of topographic features. When measuring the amount of subsidence, it is necessary to set an appropriate amount of reference point, and the depression of the formation of each reference point can be used to draw the contour line of the depression amount, to find the center of the subsidence, and obtain the comparison results of multiple times to find out The formation is trapped under time. However, this method is quite labor-intensive and time-consuming, and the measurement interval is large, and the average side can be measured once every two to three months, and it is difficult to obtain continuous formation subsidence data.

除了上述地表面傳統偵測方式之外,地下監測可分為單點式或多點式,單點式指的是量測監測井中固定位置的沉陷變化,詳細來說,一般會以監測井的底部作為固定量測點,再以裝設在地表或量測井內之地層的監測儀器,量測地層目前的深度,以比較原先深度來產生的沉陷值。In addition to the above-mentioned traditional surface detection methods, underground monitoring can be divided into single-point or multi-point, single-point refers to the measurement of the subsidence change in the fixed position in the monitoring well. In detail, the monitoring well is generally The bottom is used as a fixed measuring point, and the current depth of the stratum is measured by a monitoring instrument installed in the ground or measuring well to compare the sinking value generated by the original depth.

多點式可分為兩種,其中一種係靠設置伸張儀置入監測井內,並灌入水泥和皂土混合漿,固結後即可量測。當地層發生下陷時,伸張儀內彈性鋼伸縮桿在尼龍質保護管內滑動,其位移量顯示該點至地表之壓縮量,於地表以游標尺測定位移量。多點式的另一種則採用磁性環配合量測管放置於地下不同深度,然後透過銦鋼尺加上磁性探測器,於量測管下放探測磁性環位置,藉以確認不同時間下之位置差異,即為該深度點之沉陷值。The multi-point type can be divided into two types, one of which is placed in the monitoring well by setting the extensometer, and is poured into the mixed slurry of cement and bentonite, and can be measured after consolidation. When the local layer is sunken, the elastic steel telescopic rod in the extension gauge slides in the nylon protective tube, and the displacement shows the compression amount from the point to the surface, and the displacement is measured on the surface by the vernier scale. The other one of the multi-point type uses a magnetic ring with a measuring tube placed at different depths in the ground, and then a magnetic detector is placed through the indium steel ruler to detect the position of the magnetic ring under the measuring tube, thereby confirming the position difference at different times. This is the sink value of the depth point.

但無論是單點式或多點式的量測方式,其事前所需安裝的手續皆相當繁複,且必須採用人為操作才可進行監測,無法使用儀器不間斷的即時反映出每個時間點土壤的沉陷的變化。再者,除了地層下陷所須蒐集的數值除了土壤沉陷量之外,監測井中水壓的數據也相當的重要。目前量測水壓的方式是額外再鑽出一個監測井,並放入水壓計量測水壓,因此傳統水壓量測方法並無法在一地點,量測水壓以及土壤的沉陷量,導致數據之間可能因地點不同等因素,使蒐集的參數不完整,造成後續資料所演算出數據不準確。However, whether it is a single-point or multi-point measurement method, the procedures required for the installation beforehand are quite complicated, and must be monitored by human operation. The instrument cannot be used to reflect the soil at each time point without interruption. The change of subsidence. Furthermore, in addition to the amount of soil subsidence, in addition to the amount of soil subsidence, the data on monitoring the water pressure in the well is also very important. At present, the way to measure the water pressure is to additionally drill a monitoring well and put it into the water pressure to measure the water pressure. Therefore, the traditional water pressure measurement method cannot measure the water pressure and the amount of soil subsidence at a place. The factors that may result in different data may be incomplete, and the collected parameters are incomplete, resulting in inaccurate data calculated by subsequent data.

有鑑於此,本發明遂針對上述習知技術之缺失,提出一種時域反射式監測沉陷變化裝置及其方法,以有效克服上述之該等問題。In view of the above, the present invention has been directed to the absence of the above-mentioned prior art, and proposes a time domain reflective monitoring subsidence changing device and method thereof to effectively overcome the above problems.

本發明之主要目的在提供一種時域反射式監測沉陷變化裝置及其方法,其利用時域反射之電磁脈波量測多點深度之土壤沉陷量,且可自動化偵測沉陷量,並可濾除原先系統中所產生的誤差值,以達到精確數值量測,係為較可靠的量測技術。The main object of the present invention is to provide a time domain reflection type monitoring subsidence changing device and a method thereof, which use the electromagnetic pulse wave reflected by the time domain to measure the soil subsidence at a multi-point depth, and can automatically detect the sinking amount, and can filter In addition to the error values generated in the original system to achieve accurate numerical measurements, it is a more reliable measurement technique.

本發明之另一目的在提供一種時域反射式監測沉陷變化裝置及其方法,其利用電磁脈波量測可達到快速量測以及量測數據精確等優點,同時可一併在量測沉陷量的同一地點中,取得水壓之參數,能避免不同地點的量測而產生誤差,有利於提升地層下陷之的演算精確度。Another object of the present invention is to provide a time domain reflection type monitoring subsidence changing device and a method thereof, which can utilize the electromagnetic pulse wave measurement to achieve the advantages of rapid measurement and accurate measurement data, and can simultaneously measure the amount of subsidence. In the same place, the parameters of the water pressure can avoid errors in the measurement of different places, which is beneficial to improve the calculation accuracy of the subsidence of the formation.

為達上述之目的,本發明提供一種時域反射式監測沉陷變化裝置,其係安裝在一待測環境中,以監測待測環境的土壤沉陷變化量,其中時域反射式監測沉陷變化裝置包括至少一傳輸線,傳輸線的一內導體連接至少一同軸纜線,傳輸線的一外導體則連接一導電管體,且傳輸線可傳送一電磁脈波至同軸纜線及導電管體;其中導電管體設置於待測環境中,同軸纜線則穿設在導電管體中,使傳輸線傳送的電磁脈波在導電管體中流動,導電管體內更設有至少一感測裝置,感測裝置的外表面設有至少一錨定器,錨定器穿設出導電管體,以將感測裝置固定在待監測環境之土壤;導電管體內更設有至少一水壓計,以偵測待監測環境之液體,產生一水壓訊號;至少一資料處理器電性連接水壓計以及傳輸線,資料處理器可接收水壓訊號,並控制傳輸線發出電磁脈波,且資料處理器更可透過傳輸線感測電磁脈波觸碰到感測裝置以及水壓計,所產生的一量測波形,資料處理器再擷比對量測波形與資料處理器中的一參考波形,以取得一波形時間差值後,再將波形時間差值帶入一實際沉陷量方程式中,將波形時間差值轉換成一實際沉陷量。 To achieve the above object, the present invention provides a time domain reflective monitoring subsidence changing device installed in an environment to be tested to monitor the amount of soil subsidence change of the environment to be tested, wherein the time domain reflective monitoring subsidence changing device includes At least one transmission line, an inner conductor of the transmission line is connected to at least one coaxial cable, and an outer conductor of the transmission line is connected to a conductive tube body, and the transmission line can transmit an electromagnetic pulse wave to the coaxial cable and the conductive tube body; wherein the conductive tube body is disposed In the environment to be tested, the coaxial cable is disposed in the conductive tube body, so that the electromagnetic pulse wave transmitted by the transmission line flows in the conductive tube body, and at least one sensing device is further disposed in the conductive tube body, and the outer surface of the sensing device is The anchoring device is provided with at least one anchoring device, and the anchoring device is disposed to fix the sensing device to the soil of the environment to be monitored; and the conductive tube body is further provided with at least one water pressure gauge to detect the environment to be monitored. The liquid generates a water pressure signal; at least one data processor is electrically connected to the water pressure gauge and the transmission line, and the data processor can receive the water pressure signal and control the transmission line to emit electromagnetic pulse waves, and The material processor can sense the electromagnetic pulse wave touches the sensing device and the water pressure gauge through the transmission line, and generates a measurement waveform, and the data processor compares the measurement waveform with a reference waveform in the data processor. After obtaining a waveform time difference, the waveform time difference is brought into an actual sinking amount equation, and the waveform time difference is converted into an actual sinking amount.

另外,本發明亦提供一種時域反射式監測沉陷變化方法,其包括下列步驟,首先擷取一量測波形,量測波形包括一量測基準波段以及一量測沉陷波段;接著比對量測波形之量測基準波段,與一參考波形之一參考基準波段,以取得一誤差值;再比對量測波形之量測沉陷波段,以及參考波形之一參考沉陷波段,以產生一沉陷差值;最後根據誤差值及沉陷差值之差異量,產生形成一波形時間差值,並帶入一實際沉陷量方程式,以取得一實際沉陷量。其中實際沉陷量方程式為: △S係為實際沉陷量;(△T 2-△T 1)為波形時間差值;△T 2量測器所偵測到的沉陷差值;△T 1係為水壓計的誤差質;c為光速;ε m 為導電管體內之介質的介電度;a係為量測效能比例係數;ε c 為同軸纜線之絕緣層的介電度。 In addition, the present invention also provides a time domain reflective monitoring subsidence variation method, which includes the following steps: first, a measurement waveform is selected, and the measurement waveform includes a measurement reference band and a measurement subsidence band; and then the comparison measurement The reference band of the waveform is measured, and one of the reference waveforms is referenced to the reference band to obtain an error value; the measured sinking band is compared with the measured waveform, and one of the reference waveforms is referenced to the sinking band to generate a sinking difference Finally, according to the difference between the error value and the sinking difference, a waveform time difference is generated and brought into an actual sinking amount equation to obtain an actual sinking amount. The actual subsidence equation is: △S is the actual amount of subsidence; (△ T 2 -△ T 1 ) is the waveform time difference; Δ T 2 detector detects the difference in subsidence; △ T 1 is the error quality of the water pressure gauge; c is the speed of light; ε m is the dielectric of the medium in the conductive tube; a is the measurement efficiency proportional coefficient; ε c is the dielectric of the insulating layer of the coaxial cable.

底下藉由具體實施例詳加說明,當更容易瞭解本發明之目的、技術內容、特點及其所達成之功效。 The purpose, technical content, features and effects achieved by the present invention will be more readily understood by the detailed description of the embodiments.

請參照第一圖與第二圖,本發明之時域反射式監測沉陷變化裝置1係安裝於一待監測環境中,本實施例舉例待測環境為地下水之監測井60,以監測其土壤沉陷變化量以及監測井60中的水壓變化,本實施例之在土壤62鑿出一監測井60,且監測井60的開口上設有一蓋體66,供安裝時域反射式監測沉陷變化裝置1。其中時域反射式監測沉陷變化裝置1包括,一資料處理器10、一導電管體20、至少一時域反射式的感測裝置30以及一水壓計40。其中資料處理器10設置在監測井60之蓋體66上,且電性連接至少一傳輸線12;導電管體20則設置在蓋體66上,且伸入監測井60中直接插入監測井60的土壤62中,並使土壤62內的地下水可滲入導電管體20中,導電管體20電性連接傳輸線12,導電管體20內更設有一同軸纜線22,其包括一導體222,其外表面更包覆有一絕緣層224,此絕緣層224可有效減緩地下水造成之電磁波能量衰減問題,同軸纜線22亦電性連接傳輸線12,請配合參照第三圖,以進一步詳細說明導電管體20之構造,其中導電管體20可為鋁管、銅管等金屬或可導電材質管體,且導電管體20至少一側更設有一開槽24,使土壤62內的地下水亦可由開槽24滲入導電管體20中。Referring to the first figure and the second figure, the time domain reflection type monitoring subsidence changing device 1 of the present invention is installed in a to-be-monitored environment. In this embodiment, the environment to be tested is a groundwater monitoring well 60 to monitor the soil subsidence. The change amount and the water pressure change in the monitoring well 60, in the present embodiment, a monitoring well 60 is drilled in the soil 62, and a cover 66 is provided on the opening of the monitoring well 60 for installing the time domain reflective monitoring subsidence changing device 1 . The time domain reflective monitoring subsidence changing device 1 includes a data processor 10, a conductive tube body 20, at least one time domain reflective sensing device 30, and a water pressure gauge 40. The data processor 10 is disposed on the cover 66 of the monitoring well 60 and electrically connected to at least one transmission line 12; the conductive tube 20 is disposed on the cover 66 and extends into the monitoring well 60 and directly inserted into the monitoring well 60. In the soil 62, the groundwater in the soil 62 can be infiltrated into the conductive pipe body 20. The conductive pipe body 20 is electrically connected to the transmission line 12. The conductive pipe body 20 is further provided with a coaxial cable 22, which includes a conductor 222. The surface is further covered with an insulating layer 224, which can effectively alleviate the problem of electromagnetic wave energy attenuation caused by groundwater. The coaxial cable 22 is also electrically connected to the transmission line 12. Please refer to the third figure for further detailed description of the conductive tube body 20. The conductive tube body 20 can be a metal tube or a conductive material tube body such as an aluminum tube or a copper tube, and the conductive tube body 20 is further provided with a slot 24 on at least one side thereof, so that the groundwater in the soil 62 can also be slotted. It penetrates into the conductive tube body 20.

接下來請參照第一圖與第四圖,以詳細說明導電管體20、同軸纜線22以及傳輸線12的連接關係。如圖所示,資料處理器10之傳輸線12係透過設置在蓋體66上的一轉接頭14之固定環142,將傳輸線12的一內導體122連接同軸纜線22之導體222,傳輸線12的外導體124則連接導電管體20,使資料處理器10能控制傳輸線12傳送一電磁脈波至同軸纜線22及導電管體20之間,使電磁脈波在導電管體20中流動。Next, please refer to the first and fourth figures to explain in detail the connection relationship between the conductive tube body 20, the coaxial cable 22, and the transmission line 12. As shown, the transmission line 12 of the data processor 10 connects an inner conductor 122 of the transmission line 12 to the conductor 222 of the coaxial cable 22 through a fixing ring 142 of a connector 14 disposed on the cover 66. The transmission line 12 The outer conductor 124 is connected to the conductive tube body 20, so that the data processor 10 can control the transmission line 12 to transmit an electromagnetic pulse wave between the coaxial cable 22 and the conductive tube body 20, so that the electromagnetic pulse wave flows in the conductive tube body 20.

請回復參照第一圖與第二圖,感測裝置30設置在導電管體20內,本發明可串接多個感測裝置30在導電管體20內,本實施例僅以一個感測裝置30作為舉例說明,但不以設置一個感測裝置30為限制,同軸纜線22則穿過感測裝置30,感測裝置30係為活動式的,可在導電管體20內移動,感測裝置30外表包含一錨定器34,錨定器34可穿設出導電管體20的開槽24,以將感測裝置30固定在土壤62,由於感測裝置30可在導電管體20內移動,且固定在土壤62上,因此當土壤62下陷時感測裝置30就能跟著土壤62一起下陷,使感測裝置30的目前所在的位置能作為量測下陷的基準;導電管體20內更設有一置中器26,使同軸纜線22穿設於置中器26中,將同軸纜線22及感測裝置30置中在導電管體20中,以提升量測波形穩定性。本實施例舉例感測裝置30包括有一金屬感測器36以及一非金屬感測器38,金屬感測器36之材料係為鋁、銅或其他導電之材質,非金屬感測器38之材料則為塑膠、聚苯乙烯或不可導電之材質;金屬感測器36與非金屬感測器38係串接在一起,且金屬感測器36位於非金屬感測器38的上方,當導電管體20中的電磁脈波觸碰到金屬感測器36與非金屬感測器38時,可產生不同的波形變化,以利用此波形的變化作為特徵點,以取得金屬感測器36與非金屬感測器38在監測井60中的位置。Referring to the first and second figures, the sensing device 30 is disposed in the conductive tube body 20, and the present invention can serially connect the plurality of sensing devices 30 in the conductive tube body 20. This embodiment only uses one sensing device. 30 is exemplified, but not limited by the provision of one sensing device 30. The coaxial cable 22 passes through the sensing device 30. The sensing device 30 is movable and can be moved within the conductive tube 20 to sense The device 30 includes an anchor 34. The anchor 34 can pass through the slot 24 of the conductive tube 20 to fix the sensing device 30 to the soil 62. Since the sensing device 30 can be in the conductive tube 20 Moving and fixed on the soil 62, the sensing device 30 can be sunk together with the soil 62 when the soil 62 sinks, so that the current position of the sensing device 30 can be used as a reference for measuring the subsidence; the conductive tube body 20 A centering device 26 is further disposed to allow the coaxial cable 22 to pass through the centering device 26, and the coaxial cable 22 and the sensing device 30 are centered in the conductive tube body 20 to improve the stability of the measured waveform. In this embodiment, the sensing device 30 includes a metal sensor 36 and a non-metal sensor 38. The material of the metal sensor 36 is aluminum, copper or other conductive material, and the material of the non-metal sensor 38. The material is plastic, polystyrene or non-conductive material; the metal sensor 36 is connected in series with the non-metal sensor 38, and the metal sensor 36 is located above the non-metal sensor 38, when the conductive tube When the electromagnetic pulse wave in the body 20 touches the metal sensor 36 and the non-metal sensor 38, different waveform changes can be generated to utilize the change of the waveform as a feature point to obtain the metal sensor 36 and the non-metal sensor 36 Metal sensor 38 is in position in monitoring well 60.

水壓計40亦設置在導電管體20內,以偵測從土壤中滲進導電管體20內的地下水水壓,且水壓計40更電性連接一類比轉換器42,類比轉換器42再電性連接至資料處理器10。水壓計40能偵測待環境中液體的水壓,產生一水壓訊號,並將水壓訊號傳遞給類比轉換器42經訊號轉換後,再傳遞給資料處理器10。當導電管體20內的電磁脈波觸碰到水壓計40時,亦可產生不同的波形變化,本發明則可利用此波形的變化作為特徵點,以取得水壓計40的位置。The water pressure gauge 40 is also disposed in the conductive tube body 20 to detect the groundwater pressure in the conductive tube body 20 from the soil, and the water pressure gauge 40 is electrically connected to the analog converter 42, the analog converter 42. Re-electrically connected to the data processor 10. The water pressure gauge 40 can detect the water pressure of the liquid in the environment, generate a water pressure signal, and transmit the water pressure signal to the analog converter 42 for signal conversion, and then to the data processor 10. When the electromagnetic pulse wave in the conductive pipe body 20 touches the water pressure gauge 40, different waveform changes can also be generated, and the present invention can use the change of the waveform as a feature point to obtain the position of the water pressure gauge 40.

接下來請持續參照第一圖與第二圖,以詳細說明資料處理器10之結構,資料處理器10更包括一時域反射儀16以及一計算機18,其中時域反射儀16電性連接傳輸線12,以發出電磁脈波至傳輸線12,並透過傳輸線12接收量測波形。計算機18則電性連接時域反射儀16以及類比轉換器42,計算機18可接收時域反射儀16的量測波形,以及類比轉換器42所轉換之水壓計40的水壓訊號,並顯示水壓訊號於電性連接計算機18的一顯示器19中給使用者參考;計算機18內更儲存有一參考波形,以及一實際沉陷量方程式,計算機透過傳輸線12感測電磁脈波觸碰到感測裝置30以及水壓計40所產生的量測波形,以比對量測波形與參考波形,取得一波形時間差值後,再帶入實際沉陷量方程式中,將波形時間差值轉換成一實際沉陷量,並在顯示器19中顯示實際沉陷量。The structure of the data processor 10 is further described in detail with reference to the first and second figures. The data processor 10 further includes a time domain reflectometer 16 and a computer 18, wherein the time domain reflectometer 16 is electrically connected to the transmission line 12. To emit an electromagnetic pulse wave to the transmission line 12 and receive the measurement waveform through the transmission line 12. The computer 18 is electrically connected to the time domain reflectometer 16 and the analog converter 42. The computer 18 can receive the measurement waveform of the time domain reflectometer 16 and the water pressure signal of the water pressure gauge 40 converted by the analog converter 42 and display The water pressure signal is referenced to a user in a display 19 of the electrical connection computer 18; the computer 18 further stores a reference waveform and an actual sinking amount equation, and the computer senses the electromagnetic pulse wave through the transmission line 12 to touch the sensing device. 30 and the measurement waveform generated by the water pressure gauge 40, to compare the measurement waveform with the reference waveform, obtain a waveform time difference, and then bring it into the actual sinking amount equation, and convert the waveform time difference into an actual sinking amount. And the actual amount of sinking is displayed in the display 19.

在說明完上述之結構,接續說明本發明之監測沉陷值之方法,請參照第一圖、第二圖以及第五圖。在進行量測沉陷值之前,必須先取得監測井60之土壤62尚未沉陷時的參考波形,以作為往後比對實際沉陷量的基準,參考波形的擷取係在一開始裝設時域反射式監測沉陷變化裝置1於待監測環境時,控制時域反射儀16發出量測電磁脈波至導電管體20內,電磁脈波在觸碰到導電管體20內的水壓計40以及感測裝置30後,產生波形的變化,並反射回參考波形時域反射儀16中,時域反射儀16再將參考波形儲存至計算機18中。其中參考波形包括一參考基準波段50以及一參考沉陷波段52,參考基準波段50為電磁脈波觸碰到水壓計40之波段,參考沉陷波段52則為電磁脈波觸碰到感測裝置30之波段,然而參考沉陷波段52呈現出波浪形的原因在於,本實施例的感測裝置30包括有不同材質的金屬感測器36以及非金屬感測器38,因此電磁脈波觸碰到金屬感測器36以及非金屬感測器38時,會產生不同的波形,如第五圖所示,參考沉陷波段52的上半段,往左邊方向突出的波段係為觸碰到金屬感測器36的波形,下半段往右邊方向突出的波形,則係觸碰到非金屬感測器38的波形。Having explained the above structure, the method of monitoring the sink value of the present invention will be described. Referring to the first, second and fifth figures. Before measuring the subsidence value, the reference waveform of the monitoring well 60 where the soil 62 has not been collapsed must be obtained as a reference for comparing the actual subsidence amount in the backward direction. The reference waveform is extracted at the beginning of the time domain reflection. When the monitoring subsidence changing device 1 is in the environment to be monitored, the control time domain reflectometer 16 emits a measuring electromagnetic pulse wave into the conductive pipe body 20, and the electromagnetic pulse wave touches the water pressure gauge 40 in the conductive pipe body 20 and senses After the measurement device 30, a change in waveform is generated and reflected back into the reference waveform time domain reflectometer 16, which in turn stores the reference waveform into the computer 18. The reference waveform includes a reference reference band 50 and a reference sink band 52. The reference reference band 50 is a band in which the electromagnetic pulse wave touches the water pressure gauge 40, and the reference sink band 52 is the electromagnetic pulse wave touches the sensing device 30. The reason for the fact that the reference sinking band 52 exhibits a wave shape is that the sensing device 30 of the present embodiment includes the metal sensor 36 of different materials and the non-metal sensor 38, so that the electromagnetic pulse wave touches the metal. When the sensor 36 and the non-metal sensor 38 are used, different waveforms are generated. As shown in the fifth figure, referring to the upper half of the sinker band 52, the band protruding to the left is a touch of the metal sensor. The waveform of 36, the waveform protruding to the right in the lower half, touches the waveform of the non-metallic sensor 38.

在取得參考波形後,請接續參照第一圖、第二圖以及第六圖,以詳細說明資料處理器10之計算機18係如何利用參考波形比對量測波形,計算出實際沉陷量。首先進入步驟S10,資料處理器10之時域反射儀16發出一電磁脈波至導電管體20以及同軸纜線22,使導電管體20內的電磁脈波觸碰到水壓計40以及感測裝置30後,反射量測波形給時域反射儀16擷取。請配合參照第六圖與第七圖,其中量測波形包括一量測基準波段54以及一量測沉陷波段56,量測基準波段54指的是電磁脈波觸碰到水壓計40之波段,量測沉陷波段56則是導電管體內電磁脈波觸碰到感測裝置30的波段。其中量測沉陷波段56呈現出波浪形的原因與參考沉陷波段52相同,故不重複敘述。After obtaining the reference waveform, please refer to the first, second and sixth figures in detail to explain in detail how the computer 18 of the data processor 10 uses the reference waveform to compare the measured waveforms to calculate the actual sinking amount. First, in step S10, the time domain reflectometer 16 of the data processor 10 sends an electromagnetic pulse wave to the conductive tube body 20 and the coaxial cable 22, so that the electromagnetic pulse wave in the conductive tube body 20 touches the water pressure gauge 40 and the sense After the measuring device 30, the reflected measurement waveform is taken by the time domain reflectometer 16. Please refer to the sixth and seventh figures, wherein the measurement waveform includes a measurement reference band 54 and a measurement subsidence band 56, and the measurement reference band 54 refers to the band of the electromagnetic pulse wave touching the hydrometer 40. The measurement subsidence band 56 is a band in which the electromagnetic pulse wave in the conductive tube touches the sensing device 30. The reason why the measurement subsidence band 56 exhibits a wave shape is the same as that of the reference sink band 52, so the description is not repeated.

接下請參照步驟S12,計算機18透過時域反射儀16取得量測波形後,比對量測波形之量測基準波段54,及參考波形之參考基準波段50,以取得一誤差值。請配合第八圖,由於感測裝置30係透過錨定器34固定在土壤62,當土壤62沉陷時感測裝置30也一併跟著沉陷,因此量測波形與未沉陷時所量測到的參考波形也會有所不同,但量測波形也可能存在的誤差值。詳細來說,如第八圖所示,本實施例中的水壓計40係未移動的狀態,但資料處理器10所擷取到的量測波形中,代表水壓計40位置的量測基準波段54的位置卻下降了,表示量測波形可能因某些因素產生誤差,因此計算機18必須擷取參考波形之參考基準波段50,以及量測波形之量測基準波段54進行比對,以取得一誤差值 ,來作為校正的參數。 Next, referring to step S12, after the computer 18 obtains the measurement waveform through the time domain reflectometer 16, the reference measurement band 54 and the reference reference band 50 of the reference waveform are compared to obtain an error value. Please cooperate with the eighth figure. Since the sensing device 30 is fixed to the soil 62 through the anchor 34, the sensing device 30 is also collapsed when the soil 62 is sunk, so the measured waveform is measured when it is not collapsed. The reference waveform will also vary, but the measured waveform may also have an error value. In detail, as shown in the eighth figure, the water pressure gauge 40 in the present embodiment is in a state of not moving, but the measurement waveform taken by the data processor 10 represents the measurement of the position of the water pressure gauge 40. The position of the reference band 54 is decreased, indicating that the measurement waveform may be subject to errors due to certain factors, so the computer 18 must capture the reference reference band 50 of the reference waveform and the measurement reference band 54 of the measurement waveform for comparison. Get an error value , as a parameter for correction.

接著請參照步驟S14,計算機18再比對量測波形之量測沉陷波段56,及參考波形之參考沉陷波段52,產生一沉陷差值 ,沉陷差值 係使用互相關係分析法(cross-correlation)比較量測波形之沉陷波段以及參考波形之沉陷波段,其中互相關係分析法係透過一互相關係分析法方程式計算出來,互相關係分析法方程式(1)如下所示: (1) Next, referring to step S14, the computer 18 compares the measured waveform waveform with the measured sinking band 56 and the reference sinking reference band 52 to generate a sinking difference. Subsidence difference The cross-correlation is used to compare the sinking band of the measured waveform with the sinking band of the reference waveform. The correlation analysis method is calculated by a correlation analysis equation. The correlation analysis equation (1) is as follows Shown as follows: (1)

其中 係為參考波形, 係為量測波形, 係為時間, 係為時間差。除了上述利用互相關係分析法判斷出沉陷差值 之外,更可直接在量測沉陷波段56以及參考沉陷波段52擷取相對的一特徵點來進行比對,舉例來說可以擷取參考沉陷波段52代表金屬感測器36以及非金屬感測器38的交接處作為特徵點a,以及擷取量測沉陷波段56中代表金屬感測器36以及非金屬感測器38的交接處作為特徵點b,特徵點a以及特徵點b之間的差即為沉陷差值 among them Is a reference waveform, Is a measurement waveform, For time, It is a time difference. In addition to the above-mentioned mutual correlation analysis method to determine the difference in subsidence In addition, a comparison can be made directly on the measurement subsidence band 56 and the reference subsidence band 52 to obtain a relative feature point. For example, the reference sink band 52 can be used to represent the metal sensor 36 and the non-metal sensing. The intersection of the device 38 serves as the feature point a, and the intersection of the representative metal sensor 36 and the non-metal sensor 38 in the measurement subsidence band 56 is taken as the feature point b, between the feature point a and the feature point b. Difference is the difference .

最後進入步驟S16,計算機18即可比對步驟S12所計算出的誤差值 ,及步驟S14演算出的沉陷差值 的差異,產生形成一波形時間差值 ,波形時間差值 再帶入一實際沉陷量方程式,以取得一實際沉陷量 。其中實際沉陷量方程式(2)如下所示: (2) 其中 係為實際沉陷量; 為波形時間差值; 為沉陷差值; 係為誤差值; 為光速; 為導電管體內之介質的介電度; 為一量測效能比例係數; 係為同軸纜線之絕緣層的介電度。 Finally, proceeding to step S16, the computer 18 can compare the error value calculated in step S12. And the difference in sinking calculated in step S14 Difference in waveform, resulting in a waveform time difference Waveform time difference Then bring in an actual subsidence equation to obtain an actual subsidence . The actual subsidence equation (2) is as follows: (2) where Is the actual amount of subsidence; Is the waveform time difference; For the subsidence difference; Is the error value; For the speed of light; The dielectric of the medium in the conductive tube; Measuring the performance ratio factor for a quantity; It is the dielectric of the insulating layer of the coaxial cable.

綜上所述,本發明可利用時域反射之電磁脈波,量測多點深度土壤的沉陷量,可自動化、快速並不斷偵測到每一個時間點的沉陷量,同時更可濾除原先系統中所產生的誤差值,以達到精確數值量測,係為較可靠的量測技術。除此之外,本發明更可同時一併在量測沉陷量的同一地點中,取得水壓之參數,避免不同地點產生數值上的誤差,有利於提升地層下陷之的演算精確度。In summary, the present invention can utilize the electromagnetic pulse wave reflected by the time domain to measure the subsidence of the soil at a multi-point depth, and can automatically, quickly and continuously detect the sinking amount at each time point, and at the same time, can filter out the original The error values generated in the system to achieve accurate numerical measurements are a more reliable measurement technique. In addition, the present invention can simultaneously obtain the parameters of the water pressure in the same place where the amount of subsidence is measured, avoiding numerical errors in different places, and is advantageous for improving the calculation accuracy of the formation subsidence.

唯以上所述者,僅為本發明之較佳實施例而已,並非用來限定本發明實施之範圍。故即凡依本發明申請範圍所述之特徵及精神所為之均等變化或修飾,均應包括於本發明之申請專利範圍內。The above is only the preferred embodiment of the present invention and is not intended to limit the scope of the present invention. Therefore, any changes or modifications of the features and spirits of the present invention should be included in the scope of the present invention.

1‧‧‧時域反射式監測沉陷變化裝置1‧‧‧ Time Domain Reflective Monitoring Subsidence Change Device

10‧‧‧資料處理器10‧‧‧data processor

12‧‧‧傳輸線12‧‧‧ transmission line

122‧‧‧內導體122‧‧‧ Inner conductor

124‧‧‧外導體124‧‧‧Outer conductor

14‧‧‧轉接頭14‧‧‧Adapter

142‧‧‧固定環142‧‧‧Fixed ring

16‧‧‧時域反射儀16‧‧‧Time Domain Reflectometer

18‧‧‧計算機18‧‧‧ computer

19‧‧‧顯示器19‧‧‧ Display

20‧‧‧導電管體20‧‧‧Electrical tube body

22‧‧‧同軸纜線22‧‧‧ coaxial cable

222‧‧‧導體222‧‧‧ conductor

224‧‧‧絕緣層224‧‧‧Insulation

24‧‧‧開槽24‧‧‧ slotting

26‧‧‧置中器26‧‧‧ centering device

30‧‧‧感測裝置30‧‧‧Sensing device

34‧‧‧錨定器34‧‧‧ anchor

36‧‧‧金屬感測器36‧‧‧Metal sensor

38‧‧‧非金屬感測器38‧‧‧Non-metal sensor

40‧‧‧水壓計40‧‧‧Hydraulic pressure gauge

42‧‧‧類比轉換器42‧‧‧ analog converter

50‧‧‧參考基準波段50‧‧‧Reference reference band

52‧‧‧參考沉陷波段52‧‧‧Refer to the subsidence band

54‧‧‧量測基準波段54‧‧‧Measured reference band

56‧‧‧量測沉陷波段56‧‧‧Measure the subsidence band

60‧‧‧監測井60‧‧‧Monitoring well

62‧‧‧土壤62‧‧‧ soil

66‧‧‧蓋體66‧‧‧ cover

a‧‧‧特徵點a‧‧‧Feature points

b‧‧‧特徵點b‧‧‧Feature points

第一圖係為本發明之時域反射式監測沉陷變化裝置裝設示意圖。 The first figure is a schematic diagram of the installation of the time domain reflective monitoring subsidence changing device of the present invention.

第二圖係為本發明之時域反射式監測沉陷變化裝置方塊圖。 The second figure is a block diagram of the time domain reflective monitoring subsidence changing device of the present invention.

第三圖係為本發明之導電管體立體示意圖。 The third figure is a three-dimensional schematic view of the conductive tube body of the present invention.

第四圖係為本發明之導電管體、同軸纜線以及傳輸線的連接關係示意圖。 The fourth figure is a schematic diagram of the connection relationship of the conductive tube body, the coaxial cable and the transmission line of the present invention.

第五圖係為本發明之參考波形示意圖。 The fifth figure is a schematic waveform diagram of the present invention.

第六圖係為本發明計算實際沉陷量之步驟流程圖。 The sixth figure is a flow chart of the steps of calculating the actual sinking amount according to the present invention.

第七圖係為本發明之量測波形示意圖。 The seventh figure is a schematic diagram of the measurement waveform of the present invention.

第八圖係為本發明計算實際沉陷量方法示意圖。 The eighth figure is a schematic diagram of the method for calculating the actual sinking amount according to the present invention.

Claims (13)

一種時域反射式監測沉陷變化裝置,其係安裝於一待監測環境,以監測其土壤沉陷變化量,該時域反射式監測沉陷變化裝置包括:至少一傳輸線,其一內導體連接至少一同軸纜線,一外導體則連接一導電管體,以傳送一電磁脈波至該同軸纜線及該導電管體,其中該導電管體設置於該待測環境中,該同軸纜線則穿設在該導電管體中,使該電磁脈波在該導電管體中流動;至少一感測裝置,設置於該導電管體內,該感測裝置外表面設有至少一錨定器,該錨定器穿設出該導電管體,以將該感測裝置固定在該待監測環境之該土壤;至少一水壓計,設置於該導電管體內,以偵測該待監測環境之液體,產生一水壓訊號;以及至少一資料處理器,其電性連接該水壓計以及該傳輸線,該資料處理器可接收該水壓訊號,並控制該傳輸線發出該電磁脈波,該資料處理器可透過該傳輸線感測該電磁脈波觸碰到該感測裝置以及該水壓計所產生的一量測波形,以比對該量測波形中的一量測基準波段與一參考波形之一參考基準波段,以取得一誤差值,再比對該量測波形之一量測沉陷波段以及該參考波形之一參考沉陷波段,產生一沉陷差值,並根據該誤差值及該沉陷差值之差異量,產生一波形時間差值並帶入一實際沉陷量方程式中,將該波形時間差值轉換成一實際沉陷量,其中該實際沉陷量方程式為: 其中該△S係為該實際沉陷量;該(△T 2-△T 1)為該波形時間差值;該 △T 2為該一沉陷差值;△T 1係為一誤差值;該c為光速;該ε m 為該導電管體內之介質的介電度;該a為一量測效能比例係數;該ε c 係為該同軸纜線絕緣層的介電度。 A time domain reflective monitoring subsidence changing device is installed in a to-be-monitored environment to monitor a change in soil subsidence, the time domain reflective monitoring subsidence changing device comprising: at least one transmission line, an inner conductor connected to at least one coaxial a cable, an outer conductor is connected to a conductive tube body for transmitting an electromagnetic pulse wave to the coaxial cable and the conductive tube body, wherein the conductive tube body is disposed in the environment to be tested, and the coaxial cable is disposed In the conductive tube body, the electromagnetic pulse wave flows in the conductive tube body; at least one sensing device is disposed in the conductive tube body, and at least one anchor is disposed on an outer surface of the sensing device, the anchoring The conductive tube is disposed to fix the sensing device to the soil in the environment to be monitored; at least one water pressure gauge is disposed in the conductive tube to detect the liquid in the environment to be monitored, and generate a a water pressure signal; and at least one data processor electrically connected to the water pressure gauge and the transmission line, the data processor can receive the water pressure signal, and control the transmission line to emit the electromagnetic pulse wave, the data processor can The transmission line senses that the electromagnetic pulse wave touches the sensing device and a measurement waveform generated by the water pressure gauge, and is compared with one of the measurement reference band and a reference waveform in the measurement waveform. The reference band is obtained to obtain an error value, and the subsidence band is measured by one of the measurement waveforms, and one of the reference waveforms is referenced to the subsidence band to generate a subsidence difference, and the difference between the error value and the subsidence difference is A quantity, a waveform time difference is generated and brought into an actual sinking amount equation, and the waveform time difference is converted into an actual sinking quantity, wherein the actual sinking quantity equation is: △ S wherein the system for the actual amount of settlement; the (△ T 2 - △ T 1 ) for the waveform of the time difference; △ T 2 for the difference between a sinker; △ T 1 is a system error value; the c The speed of light; the ε m is the dielectric of the medium in the conductive tube; the a is a measured performance proportional coefficient; the ε c is the dielectric of the coaxial cable insulation layer. 如請求項1所述之時域反射式監測沉陷變化裝置,其中該資料處理器更包括:一時域反射儀,電性連接該傳輸線,以發出該電磁脈波,並接收該量測波形;以及一計算機,電性連接該時域反射儀以及該水壓計,該計算機儲存該參考波形以及該實際沉陷量方程式,並接收該時域反射儀傳遞之該量測波形,以計算該實際沉陷量。 The time domain reflective monitoring subsidence changing device of claim 1, wherein the data processor further comprises: a time domain reflectometer electrically connected to the transmission line to emit the electromagnetic pulse wave and receive the measurement waveform; a computer electrically connecting the time domain reflectometer and the water pressure gauge, the computer storing the reference waveform and the actual sinking amount equation, and receiving the measured waveform transmitted by the time domain reflectometer to calculate the actual sinking amount . 如請求項1所述之時域反射式監測沉陷變化裝置,其中該量測基準波段以及該參考基準波段,為該電磁脈波觸碰到該水壓計之波段;該量測沉陷波段以及該參考沉陷波段,為該電磁脈波觸碰到該感測裝置之波段。 The time domain reflective monitoring subsidence changing device according to claim 1, wherein the measuring reference band and the reference reference band are bands in which the electromagnetic pulse wave touches the water pressure gauge; the measuring subsidence band and the Referring to the sinking band, the electromagnetic pulse wave touches the band of the sensing device. 如請求項1所述之時域反射式監測沉陷變化裝置,其中該同軸纜線更包括一導體,該導體外表面更包覆一絕緣層。 The time domain reflective monitoring subsidence changing device of claim 1, wherein the coaxial cable further comprises a conductor, and the outer surface of the conductor is further covered with an insulating layer. 如請求項1所述之時域反射式監測沉陷變化裝置,其中該沉陷差值係使用互相關係分析法(cross-correlation)比較該量測波形之該沉陷波段以及該參考波形之沉陷波段。 The time domain reflective monitoring subsidence changing device of claim 1, wherein the sinking difference is a cross-correlation comparing the sinking band of the measuring waveform with a sinking band of the reference waveform. 如請求項1所述之時域反射式監測沉陷變化裝置,其中該時域反射式感測裝置更包括一金屬感測器以及一非金屬感測器。 The time domain reflective monitoring subsidence changing device of claim 1, wherein the time domain reflective sensing device further comprises a metal sensor and a non-metal sensor. 如請求項6所述之時域反射式監測沉陷變化裝置,其中該金屬感測器之材料係為鋁、銅或其他導電之材質。 The time domain reflective monitoring subsidence changing device according to claim 6, wherein the material of the metal sensor is aluminum, copper or other conductive material. 如請求項6所述之時域反射式監測沉陷變化裝置,其中該非金屬感測 器之材料係為塑膠、聚苯乙烯或不可導電之材質。 The time domain reflective monitoring subsidence changing device according to claim 6, wherein the non-metal sensing The material of the device is plastic, polystyrene or non-conductive material. 如請求項1所述之時域反射式監測沉陷變化裝置,更包括一置中器設置於該導電管體內,且該同軸纜線穿設於該置中器中,使該同軸纜線及該感測裝置可置中在該導電管體中。 The time domain reflective monitoring subsidence changing device of claim 1, further comprising a centering device disposed in the conductive tube body, wherein the coaxial cable is disposed in the centering device to enable the coaxial cable and the coaxial cable A sensing device can be centered in the conductive tube. 如請求項1所述之時域反射式監測沉陷變化裝置,其中該導電管體係為金屬管體,其可為鋁管或銅管。 The time domain reflective monitoring subsidence changing device of claim 1, wherein the conductive tube system is a metal tube body, which may be an aluminum tube or a copper tube. 如請求項1所述之時域反射式監測沉陷變化裝置,其中該導電管體之其中一側更設有至少一開槽,以供該錨定器穿設出該導電管體之該開槽,將該感測裝置固定在該待監測環境之該土壤。 The time domain reflective monitoring subsidence changing device of claim 1, wherein one side of the conductive tube body is further provided with at least one slot for the anchor to pass through the slot of the conductive tube body. And fixing the sensing device to the soil in the environment to be monitored. 一種時域反射式監測沉陷變化方法,包括下列步驟:擷取一量測波形,該量測波形包括一量測基準波段以及一量測沉陷波段;比對該量測波形之該量測基準波段,及一參考波形之一參考基準波段,以取得一誤差值;比對該量測波形之該量測沉陷波段,及該參考波形之一參考沉陷波段,產生一沉陷差值;以及根據該誤差值及該沉陷差值之差異量,產生一波形時間差值,並帶入一實際沉陷量方程式,以取得一實際沉陷量,其中該實際沉陷量方程式為: 其中該△S係為該實際沉陷量;該(△T 2-△T 1)為該波形時間差值;該△T 2該沉陷差值;△T 1係為該誤差值;該c為光速;該ε m 為該導電管體內之介質的介電度;該a係為一量測效能比例係數;該ε c 為該 同軸纜線之絕緣層的介電度。 A time domain reflective monitoring subsidence variation method includes the following steps: capturing a measurement waveform, the measurement waveform includes a measurement reference band and a measurement subsidence band; and the measurement reference band of the measurement waveform And one of the reference waveforms is referenced to the reference band to obtain an error value; the measured subsidence band is compared to the measurement waveform, and one of the reference waveforms refers to the subsidence band to generate a subsidence difference; and according to the error The difference between the value and the subsidence difference produces a waveform time difference and is brought into an actual subsidence equation to obtain an actual subsidence amount, wherein the actual subsidence equation is: Wherein the ΔS is the actual sinking amount; the (Δ T 2 - Δ T 1 ) is the waveform time difference; the Δ T 2 the sinking difference; Δ T 1 is the error value; the c is the speed of light The ε m is the dielectric of the medium in the conductive tube; the a is a measured performance ratio coefficient; the ε c is the dielectric of the insulating layer of the coaxial cable. 如請求項12所述之時域反射式監測沉陷變化方法,其中該沉陷差值係使用互相關係分析法(cross-correlation)比較該量測波形之該沉陷波段以及該參考波形之沉陷波段。 The time domain reflective monitoring subsidence variation method of claim 12, wherein the sinking difference is a cross-correlation comparing the sinking band of the measured waveform with a sinking band of the reference waveform.
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