• 대한원격탐사학회지
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• 제17권2호
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• pp.141-153
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• 2001

A semi-empirical polarimetric backscattering model for bare soil surfaces is presented. Based on measurements by using polarimetric scatterometers and the JPL AirSAR, as well as the theoretical models, the backscattering coefficints $\sigma$$^0_w$, $\sigma$$^0_{hh}$ and $\sigma$$^0_{vh}$, and the parameters of the copolarized phase-difference probability density function, namely the degree of correlation $\alpha$ and the copolarized-phase-difference $\zeta$, are modeled empirically in terms of the volumetric soil moisture content m$_v$ and the surface roughness parameters $k_s$ and $k_l$, where k=2$\pi$f/c, s is the rms height and l is the correlation length.

• 한국전자파학회논문지
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• 제17권12호
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• pp.1181-1188
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• 2006

본 논문에서는 토양 표면의 레이더 후방 산란 계수와 표면 거칠기의 관계를 계산해 보고, 측정 길이에 따른 표면 거칠기 변화를 알아본 후에, 측정 길이에 따른 표면 거칠기와 레이더 후방 산란 계수의 관계를 보여준다. 이 연구 결과에 따르면, 측정 길이가 짧아져서 표면 거칠기 값의 변화가 심하다하더라도 계산된 레이더 후방 산란 계수에는 적은 영향밖에 주지 않는다는 것을 보여준다.

• 한국농공학회지
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• 제15권1호
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• pp.2913-2924
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• 1973

이와같은 방법(方法)에 의(依)하여 얻은 몇가지 시험결과(試驗結果)를 요약(要約)하면 다음과 같다. 1. 어느 시험구(試驗區)를 막론(莫論)하고 건조진행(乾燥進行)은 표층토(表層土)가 라지구(裸地區)보다는 초지구(草地區)가 그 진행속도(進行速度)가 좀빠른 경향(傾向)을 나타냈다. 2. 건조과정(乾燥過程)에 강우(降雨)가 있으며 토양수분(土壤水分)은 강우침투경로(降雨浸透經路)를 통(通)하여 포장용수량(圃場容水量) 또는 수분당량(水分當量) 부근(附近)으로 회복(回復)하고 있다. 3. 성층토양(成層土壤)에서 하층토(下層土)의 토성(土性)이 상층토(上層土)의 건조(乾燥)에 미치는 영향(影響)은 다음과 같이 설명(說明)된다. 가. 하층토(下層土)가 S이고 토층토(土層土)가 CL 또는 SL인 경우에 이 CL 또는 SL의 건조(乾燥)는 포장용수량(圃場容水量)이 적은 하층(下層)의 S가 어느정도(程度) 모관수공급(毛管水供給)의 차단층(遮斷層)이 되어 하층토(下層土)가 SL 또는 CL로 되었을 때보다 훨씬 건조(乾燥)가 빨리 진행(進行)하며 CL보다는 SL쪽이 현저(顯著)하게 빨리 건조(乾燥)한다. 나. 하층토(下層土)가 SL이고 상층토(上層土)가 S 또는 SL인경우에 이 S 또는 CL의 건조(乾燥)는 포장용수량(圃場容水量)이 비교적(比較的) 크고 또 모관수전도도(毛管水傳導度)도 비교적(比較的) 원활(圓滑)한 하층(下層)의 SL로 인(因)하여 그 진행속도(進行速度)가 가장 완만하며 S보다는 CL쪽이 더빨리 건조(乾燥)하는 경향(傾向)이다. 다. 하층토(下層土)가 CL이고 상층토(上層土)가 S 또는 SL인 경우에 이 S 또는 SL의 건조(乾燥)는 포장용수량(圃場容水量)이 가장 크나 모관수전도도(毛管水傳導度)가 가장느린 하층(下層)의 CL로 인(因)하여 그 진행속도(進行速度)가 비교적(比較的) 빠른 편(便)이며 S보다는 SL쪽이 더 발리 건조(乾燥)하는 경향(傾向)이다. 4. 상층토양(上層土壤) 및 하층토양(下層土壤)에서의 함수비(含水比)에 대(對)한 1일간(日間)의 시간적(時間的) 변화(變化)를 보면 상층토양(上層土壤)이 CL 및 SL에 있어서는 기온(氣溫)이 상승(上昇)하는 $12{\sim}15$시(時) 사이 까지는 함수비(含水比)가 감소(減少)되고 18시(時) 이후(以後)부터는 약간(若干) 회복(回復)하는 경향(傾向)을 보이는데 이에 반(反)하여 S에 있어서는 기온(氣溫)이 상승(上昇)하는 $12{\sim}15$시(時)에 함수비(含水比)가 Peak점(點)을 이루는 경향(傾向)을 보였으며 하층토양(下層土壤)에서의 함수비(含水比)는 CL, SL 및 S모두 기온상승(氣溫上昇)에 따라서 약간감소(若干減少)하는 경향(傾向)을 나타냈고 구름낀날의 함수비(含水比)의 변화(變化)는 CL, SL 및 S공(共)히 맑은 날에 비(比)하여 약간(若干) 작은 경향(傾向)을 보였다. 5. 적산계기증발량(積算計蒸發量)에 대(對)한 적산토양수분소비율(積算土壤水分消費率)은 일반적(一般的)으로 화지구(華地區)가 라지구(裸地區)보다 큰 경향(傾向)을 보였으며 시일(時日)의 경과(經過)에 따라 그 율(率)이 감소(減少)하는 경향(傾向)을 보였고 또 그것은 초기(初期)에는 주(主)로 상층토양(上層土壤)의 토성(土性)에 좌우(左右)되고 후기(後期)에는 하층토양(下層土壤)의 토성(土性)에 많이 좌우(左右)되는 경향(傾向)이었다. 6. 적산토양수분소비율(積算土壤水分消費率)은 하층토(下層土)가 SL 또는 S이고 상층토(上層土)가 CL인 경우(境遇)에 하층(下層)이 SL인 경우(境遇)가 S인 경우보다 변화폭(變化幅)에 컸으며, 하층(下層)이 CL, 또는 S이고 상층(上層)이 SL인 경우(境遇)는 가장 큰 값을 나타냈는데 하층(下層)이 CL인 소우(塑遇)의 그 값은 S인 경우보다 약간(若干)큰 경향(傾向)을 보였다. 또한 하층(下層)이 CL 또는 SL이고 상층(上層)이 S인 경우는 위에 말한 두 경우보다도 작은 값을 보였으며 하층(下層)이 CL인 경우(境遇)가 SL인 경우보다 더욱더 작은 값을 나타내는 경향(傾向)을 보였으며, 즉(卽) 본시험(本試驗)에서의 토양수분(土壤水分) 소비율(消費率)은 대체(大體)로 SL/CC> SL/S>CL/SL> CL/S$\fallingdotseq$S/SL> S/CL>의 순위(順位)로 되었다.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2005년도 Proceedings of ISRS 2005
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• pp.221-224
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• 2005

Hyperspectral image data have great potential to depict more detailed information on biophysical characteristics of surface materials, which are not usually available with multispectral data. This study aims to test the potential of hyperspectral data for classifying five soil classes defined by the vector product interim terrain data (VITD). In this study, we try to classify surface materials of bare soil over the study area in Korea using both hyperspectral and multispectral image data. Training and test samples for classification are selected with using VITD vector map. The spectral angle mapper (SAM) method is applied to the EO-I Hyperion data and Landsat ETM+ data, that has been radiometrically corrected and geo-rectified. Higher classification accuracy is obtained with the hyperspectral data for classifying five soil classes of gravel, evaporites, inorganic silt and sand.

• 아시안잔디학회지
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• 제4권1호
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• pp.42-48
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• 1990

Experiments were conducted to investigate the soil freezing depth and pattern with freezing measuring instruments during 1988-l989 winter season in Kangwon province. Freezing measuring instrument was made with acrylic pipes which were consisted of inner and outer parts. Inner pipe was filled with 0.01 % methylene blue solution and rubber hose to protect pipe breakdown by solution freezing. Freezing measurements were carried out by observing discoloration of methylene blue solution. Moisture content of evergreen trees and ground cover plants was also examined in the winter season. The observed results are as follows: 1.In the land of I OOM above sea level, soil freezing depth became deeper as the sum of Accumulated degree-days of temperature below 0˚C(0˚C . day) increased: Soil freezing depth was 30-40cm at l00˚C, 42-43cm at 150˚C, and 47cm at 200˚C day 2.Soil freezing with vinyl mulching was less developed by l3cm at l00˚C with sum of subzero temperature, by l7cm at 200˚C than that of the bare ground. Soil of rich hulls mulching with 4Ocm was not frozen until soil freezing at the bare ground was developed to 25cm depth. 3.Cashmeron mulching was more effective than felt mulching in the heat insulation of soil. 4.Thawing of soil was done from the lowest part of the frozen in the ground to upward in the beginning and after that it was done from the surface of frozen soil to downward. Finally thawing was completed at the middle of frozen soil.

• 대한원격탐사학회지
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• 제39권1호
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• pp.99-110
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• 2023

Land surface temperature (LST) is a critical environmental indicator affected by land cover (LC) changes. Currently, the most convenient and fastest way to retrieve LST is to use remote sensing images due to their continuous monitoring of the Earth's surface. The work intended to investigate land cover change and temperature response inAn-Najaf province. Landsat multispectral imageries acquired inAugust 1989, 2004, and 2021 were employed to estimate land cover change and LST responses. The findings exhibited an increase in water bodies, built-up areas, plantations, and croplands by 7.78%, 7.27%, 6.98%, 3.24%, and 7.78%, respectively, while bare soil decreased by 25.27% for the period (1989-2021). This indicates a transition from barren lands to different land cover types. The contribution index (CI) was employed to depict how changes in land cover categories altered mean region surface temperatures. The highest LSTs recorded were in bare lands (42.2℃, 44.25℃, and 46.9℃), followed by built-up zones (41.6℃, 43.96℃, and 44.89℃), cropland (30.9℃, 32.96℃, and 34.76℃), plantations (35.4℃, 36.97℃, and 38.92℃), and water bodies (27.3℃, 29.35℃, and 29.68℃) respectively, in 1989, 2004, and 2021. Consequently, these changes resulted in significant variances in LST between different LC types.

• 물과 미래
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• 제5권2호
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• pp.44-48
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• 1972

This article includes hydrometeorological analysis of evapotranspiration and precipitation, which are used available basic data for a certain basin water budget. Evapotranspiration on water surface, bare soil and rice fields is directly measured by Thornthwaite's type Lysimeter and on water surface and vegetables computed using the Penman's equation. Areal precipitation is analized through the Thiessen method and arithmatic mean method. It is interested fact that the correlation coefficient for Class A Pan's evaporation vs. the actual evapotranspiration is the highest value among the coefficients for different type evaporimeter and Penman equation, and evaporation ratio on rice field's evapotranspiration vs. Class A Pan's evaporation is 1. 5-2. 3.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 1999년도 Proceedings of International Symposium on Remote Sensing
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• pp.154-157
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• 1999

Microwave polarimetric backscattering from a wet soil surface had been measured using a Ku-band polarimetric scatterometer at the incidence angles ranging from 10$^{\circ}$ to 70$^{\circ}$ Since the accurate target parameters as well as the radar parameters are necessary for radar scattering modeling, a complete and accurate set of ground truth data were also collected, from which accurate measurements were made of the rms height, correlation length, and dielectric constant. The measured polarimetric backscattering coefficients (vv-, hh-, vh-, hv-polarizations) were compared with theoretical models and empirical models. A new semi-empirical model for microwave polarimetric radar backscattering from bare soil surfaces was developed using polarimetric radar measurements and the knowledge based on the theoretical and numerical solutions. The model was found to yield very good agreement with the backscattering measurements of this study.

• 한국농공학회지
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• 제35권3호
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• pp.36-46
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• 1993

The purposes of this study are to develop three-layered Green-Ampt infiltration model considering temporal variation of physical properties of soil and to evaluate the model with field experiment on bare-tilled and soybean-growing soil plots under natural rainfalls. Infiltration tests were conducted on a sandy loam soil. The model has three-layered soil profile including a surface crust, a tilled layer, a subsoil and considers temporal variation of porosity, hydraulic conductivity, capillary pressure head on a tilled layer by natural rainfalls and canopy density variation of crop. Field measurement of porosity, average hydraulic conductivity and average capillary presure head on a tilled layer were conducted by soil sampler and air-entry permeameter at regular intervals-after tillage. It was found that temporal variation of porosity and average hydraulic conductivity might be expressed as a function of cumulative rainfall energy and average capillary pressure head might be expressed as a function of porosity of a tilled soil. The model was calibrated by an optimization technique, Hooke and Jeeves method using hourly surface runoff data. With the calibrated parameters, the model was verified satisfactorily.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.520-523
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• 2006

Whereas it is well known that the surface roughness parameters, the RMS height and the correlation length, of a natural soil surface are underestimated with a short surface profile, it is not clear how much the underestimated surface parameters affect the backscattering coefficients of the surface for various incidence angles and polarizations. The backscattering coefficients of simulated and measured surface profiles are computed using the integral equation method (IEM) and analyzed in this paper to answer this question. It is shown that the RMS error of the backscattering coefficients between 5-m- and 1-m-long measured surface profiles is 1.7 dB for vv-polarization and 0.5 dB for hh-polarization at a medium range of incidence angle ($15^{\circ}{\leq}{\theta}{\leq}70^{\circ}$), while the surface roughness parameters are significantly reduced; from 2.4 cm to 1.5 cm for the RMS height s and from 35.1 cm to 10.0 cm for the autocorrelation length l. This result is verified with numerous simulations with various roughness conditions and various wavelengths.