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RISS 인기검색어
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- 저자 : 허승오 ( Seung O Hur ) (검색결과 177 건)
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허승오,한경화,전상호,장용선,강신우,정선옥,김학진,이경환,Hur, Seung-Oh,Han, Kyeong-Hwa,Jeon, Sang-Ho,Jang, Yong-Sun,Kang, Sin-Woo,Chung, Sun-Ok,Kim, Hak-Jin,Lee, Kyeong-Hwan Institute of Agricultural Science 2011 Korean Journal of Agricultural Science Vol.38 No.4
Protected crop production has been popular in Korea as well as in other countries. Intensive and continuous monitoring and control of the environment, which is labor- and time-consuming, is critical for stable crop productivity and profitability, otherwise damage could be happened due to unfavorable ambient and soil conditions. In the study, potential utilization of smartphone and remote access application in protected crop production environment was investigated. Tested available remote access applications provided functions of mouse click (left and right buttons), zooming in and out, and screen size and color resolution control. Wi-Fi data communication speeds were affected by signal intensity and user place. Data speeds at high (> -55 dBm), medium (-70~-56 dBm), and low (< -71 dBm) signal intensity levels were statistically different (${\alpha}=0.05$). Means of data communication speed were 6.642, 4.923, and 2.906 Mbps at hot spot, home, and office, respectively, and the differences were significant at a 0.05 level. Smart phone and remote access application were applied successfully to remote monitoring (inside temperature and humidity, and outside precipitation, temperature, and humidity) and control (window and light on/off) of green house environment. Response times for monitoring and control were less than 1 s at all places for high signal intensity (> -55 dBm), but they were increased to 1 ~ 10 s at home and office and to 10 ~ 30 s at hot spot for low signal intensity (< -71 dBm) for Wi-Fi. Results of the study would provide useful information for farmers to apply these techniques for their crop production.
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허승오,류명진,류동기,정선옥,허윤근,최진용,Hur, Seung-Oh,Ryu, Myong-Jin,Ryu, Dong-Ki,Chung, Sun-Ok,Huh, Yun-Kun,Choi, Jin-Yong Institute of Agricultural Science 2011 Korean Journal of Agricultural Science Vol.38 No.4
Wireless technology has enabled farmers monitor and control protected production environment more efficiently. Utilization of USN (Ubiquitous Sensor Network) devices also brought benefits due to reduced wiring and central data handling requirements. However, wireless communication loses signal under unfavorable conditions (e.g., blocked signal path, low signal intensity). In this paper, performance of commercial wireless communication devices were evaluated for application to protected crop production. Two different models of wireless communication devices were tested. Sensors used in the study were weather units installed outside and top of a greenhouse (wind velocity and direction, precipitation, temperature and humidity), inside ambient condition units (temperature, humidity, $CO_2$, and light intensity), and irrigation status units (irrigation flow and pressure, and soil water content). Performance of wireless communication was evaluated with and without crop. For a 2.4 GHz device, communication distance was decreased by about 10% when crops were present between the transmitting and receiving antennas installed on the ground, and the best performance was obtained when the antennas were installed 2 m above the crop canopy. When tested in a greenhouse, center of a greenhouse was chosen as the location of receiving antenna. The results would provide information useful for implementation of wireless environment monitoring system for protected crop production using USN devices.
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허승오(Seung-Oh Hur),류명진(Myong-Jin Ryu),류동기(Dong-Ki Ryu),정선옥(Sun-Ok Chung),허윤근(Yun-Kun Huh),최진용(Jin-Yong Choi) 충남대학교 농업과학연구소 2011 농업과학연구 Vol.38 No.4
Wireless technology has enabled farmers monitor and control protected production environment more efficiently. Utilization of USN (Ubiquitous Sensor Network) devices also brought benefits due to reduced wiring and central data handling requirements. However, wireless communication loses signal under unfavorable conditions (e.g., blocked signal path, low signal intensity). In this paper, performance of commercial wireless communication devices were evaluated for application to protected crop production. Two different models of wireless communication devices were tested. Sensors used in the study were weather units installed outside and top of a greenhouse (wind velocity and direction, precipitation, temperature and humidity), inside ambient condition units (temperature, humidity, CO2, and light intensity), and irrigation status units (irrigation flow and pressure, and soil water content). Performance of wireless communication was evaluated with and without crop. For a 2.4 GHz device, communication distance was decreased by about 10% when crops were present between the transmitting and receiving antennas installed on the ground, and the best performance was obtained when the antennas were installed 2 m above the crop canopy. When tested in a greenhouse, center of a greenhouse was chosen as the location of receiving antenna. The results would provide information useful for implementation of wireless environment monitoring system for protected crop production using USN devices.
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허승오(Seung-Oh Hur),한경화(Kyeong-Hwa Han),전상호(Sang-Ho Jeon),장용선(Yong-Sun Jang),강신우(Sin-Woo Kang),정선옥(Sun-Ok Chung),김학진(Hak-Jin Kim),이경환(Kyeong-Hwan Lee) 충남대학교 농업과학연구소 2011 농업과학연구 Vol.38 No.4
Protected crop production has been popular in Korea as well as in other countries. Intensive and continuous monitoring and control of the environment, which is labor- and time-consuming, is critical for stable crop productivity and profitability, otherwise damage could be happened due to unfavorable ambient and soil conditions. In the study, potential utilization of smartphone and remote access application in protected crop production environment was investigated. Tested available remote access applications provided functions of mouse click (left and right buttons), zooming in and out, and screen size and color resolution control. Wi-Fi data communication speeds were affected by signal intensity and user place. Data speeds at high (> -55 dBm), medium (-70~-56 dBm), and low (< -71 dBm) signal intensity levels were statistically different (α=0.05). Means of data communication speed were 6.642, 4.923, and 2.906 Mbps at hot spot, home, and office, respectively, and the differences were significant at a 0.05 level. Smart phone and remote access application were applied successfully to remote monitoring (inside temperature and humidity, and outside precipitation, temperature, and humidity) and control (window and light on/off) of green house environment. Response times for monitoring and control were less than 1 s at all places for high signal intensity (> -55 dBm), but they were increased to 1 ~ 10 s at home and office and to 10 ~ 30 s at hot spot for low signal intensity (< -71 dBm) for Wi-Fi. Results of the study would provide useful information for farmers to apply these techniques for their crop production.
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사양토에서의 용적수분 함량 측정을 위한 TDR 및 FDR 센서의 검증
허승오(Seung-Oh Hur),하상건(Sang-Keun Ha),김정규(eong-Gyu Kim) 한국토양비료학회 2009 한국토양비료학회지 Vol.42 No.2
토양의 용적수분 함량을 현장에서 측정할 수 있어 토양 내 물 이동이나 관개관리에 효과적으로 이용할수 있는 6종의 토양수분 센서에 대한 검정을 실시했다. TDR형태의 센서가 2종으로 토양단면측정용인 TRIME과 탐침형태인 Mini-TRASE이었으며, 4종은 FDR 형태의 센서로 토양단면 측정용인 EasyAG, EnviroSCAN, PR-1과 탐침형태의 WET-1 센서였다. 코어로 측정한 용적수분함량과 비교한 결과 TRIME은 1차 선형식의 관계에서 코어측정값과 약 2.4%의 오차를 나타냈고, Mini-TRASE는 코어 용적수분함량과 약 1.4%의 오차를 나타냈으며, 이 오차는 실험에 사용했던 7종의 센서들 중에서 가장 작은 값이었다. EasyAG는 SF로 분석했을 때는 코어측정값과 약 2.6%의 오차를 나타냈고, 센서로 측정한 토양수분 함량을 코어수분함량과 직접적으로 비교했을 때도 역시 약 2.6%의 오차를 나타냈다. EnviroSCAN은 SF로 분석했을 때는 코어측정값과 약 2.8%의 오차를 나타냈고, 센서로 측정한 토양수분 함량을 코어수분 함량과 직접적으로 비교했을 때는 2.6%의 오차를 나타냈다. WET-1은 센서로 측정한 값과 코어로 실측한 값 사이에 약 2.0%의 오차가 있음을 보여주고 있으며, 이것은 검정에 사용했던 FDR 센서들 중에서는 가장 작은 값이었다. PR-1은 측정시 access 튜브 내에서 방향을 조금씩 바꿀 때마다 측정값이 달리 나오는 경우가 많아 수분함량 측정횟수가 많지 않았으나 실측값과 약 4.7%의 오차를 보였다. 결론적으로 센서의 정확성을 검정하기 위해 사용된 6종의 센서 중PR-1은 현장 측정에 문제가 있을 것으로 여겨진다. This study was to verify and calibrate seven kinds of soil water sensors for volumetric soil water content(VSWC) measurement under field. Types of sensors were TDR (Time Domain Reflectometry) and FDR(Frequency Domain Reflectometry). Two kinds of TDR were TRIME(profile type), and Mini-TRASE(rod type). Five kinds of FDR were EasyAG, EnviroSCAN, PR-1(profile type), and WET-1(rod type). VSWC by TRIME and Mini-TRASE compared with VSWC by soil core showed the standard error of about 2.4%, and 1.4% which is the smallest value among all the sensors used in the experiment, respectively. The errors of EasyAG and EnviroSCAN analyzed with scaled frequency(SF) were about 2.6%, and 2.8% and those by 1 versus 1 correspondence were about 2.6%, and 2.6%, respectively. WET-1 showed about 2.0% of error, which is the smallest value among errors by FDR sensors. PR-1 with the error of about 4.7% should be hard for application in field. Therefore, users on soil water sensors have to take into consideration the errors of sensors revealed after the calibration for the correct measurement of VSWC in field. The rest except for PR-1 among the sensors could be used for VSWC measurement with 1.4~2.6% error.
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석회암 유래 토양의 침투 및 투수속도 평가에 따른 수문유형 분류
허승오(Seung-Oh Hur),정강호(Kang-Ho Jung),손연규(Yeon-Kyu Sonn),하상건(Sang-Keun Ha),김정규(Jeong-Gyu Kim),김남원(Nam-Won Kim) 한국토양비료학회 2009 한국토양비료학회지 Vol.42 No.2
강원도 남부(영월)와 충북 제천, 단양 등지에 널리분포하는 석회암에서 유래된 토양은 점토 및 철분함량이 많은 식질계 토양이며 pH와 염기포화도(basesaturation)가 높은 붉은색 토양이다. 이 토양은 식양질과 식질 등의 세립(細粒)질로만 구성이 되어 있고자갈이 있는 토양으로 분류된다. 따라서, 토양의 침투및 투수속도가 우리나라 토양의 주 모재인 화강암이나 화강편마암 유래 토양과는 다른 양상을 보인다. 본연구는 세립질 특성을 보이는 석회암 유래 토양의 지표면에서의 침투속도와 토양층위별 투수속도를 측정해 복잡하게 세분되어 있는 토양의 종류를 수문학적 인 목적에 따라 단순화하기 위해 만든 수문학적 토양유형으로 분류하고자 하였다. 실험을 위해 이용된 토양은 과림, 모산, 장성, 마지, 안미, 평안의 6개 토양통이었고 장력 침투계(disctension infiltrometer)와 투수속도 측정계(Guelphpermeameter)로 침투 및 투수속도를 측정했다. 현장측정 이후 토양층위별로 시료를 채취하여 실험실조건에서 입도분포, 유기물함량을 측정했다. 토양통별 침투 및 투수속도를 측정한 결과는 유기물 층이 존재하는 과림통은 공극이 많고 토층 내에 나무 및 식물뿌리가 존재해 전체적으로 침투 및 투수속도가 빠른 특성을 보여 수문유형을 A로 분류하였다. 모산통은 토층 내에 자갈함량이 아주 높고 투수속도가 다른 토양에 비해 월등히 빠른 특성을 나타냈으나 50 cm이내에서 암반층이 존재하는 관계로 수문유형이 B/D로 분류되었다. 토층이 깊지 않은 장성통은 토층 내에 나무 및 식물뿌리가 많고 암석노출지가 존재해 침투속 도가 빠름에도 불구하고 C/D 수문유형으로 분류됐다. 자갈이나 잔돌이 많은 마지통은 잔자갈이 존재하고 침투나 투수속도가 빠른 편으로 B유형이었다. 논으로사용되는 안미통은 다른 석회암 유래토양에 비해 토층이 깊은 편이며 석회암 충적층에서 유래된 토양으로 선상지 및 곡간지에 분포한다. 관개된 상태에서 로타리 작업에 의해 표토의 특성이 교란되는 논으로 이용되는 특성 때문에 침투 및 투수속도는 느려 D유형으로 분류됐다. 잔돌이 존재하는 평안통은 석회암 붕적, 퇴적층으로부터 유래된 토양으로 산록경사지 및 선상단구에 분포하며 표토층인 A층에서 중 입상구조를 보이며 공극이 많고 작물뿌리가 매우 많아 침투속도는 빠르나 B층에서는 점토 함량이 감소했다 증가하면서 토성이 급격히 바뀌는 특성을 나타내 투수속도는 느린 값을 나타내 수문학적 토양유형은 D유형으로 분류됐다. Soils originated from limestone, located at the southern part of Kangwon province and Jecheon, Danyang of Chungbuk province are mainly composed of fine texture, and have different properties from soils originated from granite and granite gneiss, especially for water movement. This study was conducted for classification of hydrologic soil group (HSG) of soils originated from limestone by measuring the infiltration rate of surface soils and percolation rate of sub soils. Soils used for the experiment were 6 soils in total : Gwarim, Mosan, Jangseong, Maji, Anmi and Pyongan series. Infiltration and percolation rate were measured by a disc tension infiltrometer and a Guelph permeameter, respectively. Particle size distribution and organic matter content of the soils were analyzed. HSG, which was made by USDANRCS(National Resources Conservation Service) for hydrology, of Gwarim series with O horizon of accumulated organic matter was classified as type A which show the properties of low runoff potential, rapid infiltration and percolation rate. HSG of Mosan series, which has high gravel content and very rapid permeability, was classified as type B/D because of the impermaeble base rock layer under 50cm from surface. HSG of Jangseong series with shallow soil depth was classified as type C/D owing to the impermaeble base rock layer under 50cm from surface. HSG of Maji series was type B, and HSG of Anmi series used as paddy land was type D because of slow infiltration and percolation rate caused by the disturbance of surface soil by puddling. HSG of Pyeongan series having a sudden change of layer in soil texture was type D because of the slow percolation rate caused a the layer.
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