• 제목/요약/키워드: Soil Mapping

검색결과 210건 처리시간 0.023초

실시간 토양 유기물 센서와 DGPS를 이용한 질소 시비량 지도 작성 시스템 개발 (Development of Electronic Mapping System for N-fertilizer Dosage Using Real-time Soil Organic Matter Sensor)

  • 조성인;최상현;김유용
    • Journal of Biosystems Engineering
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    • 제27권3호
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    • pp.259-266
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    • 2002
  • It is crucial to know spatial soil variability for precision farming. However, it is time-consuming, and difficult to measure spatial soil properties. Therefore, there are needs fur sensing technology to estimate spatial soil variability, and for electronic mapping technology to store, manipulate and process the sampled data. This research was conducted to develop a real-time soil organic matter sensor and an electronic mapping system. A soil organic matter sensor was developed with a spectrophotometer in the 900∼1,700 nm range. It was designed in a penetrator type to measure reflectance of soil at 15cm depth. The signal was calibrated with organic matter content (OMC) of the soil which was sampled in the field. The OMC was measured by the Walkeley-Black method. The soil OMCs were ranged from 0.07 to 7.96%. Statistical partial least square and principle component regression analyses were used as calibration methods. Coefficient of determination, standard error prediction and bias were 0.85 0.72 and -0.13, respectively. The electronic mapping system was consisted of the soil OMC sensor, a DGPS, a database and a makeshift vehicle. An algorithm was developed to acquire data on sampling position and its OMC and to store the data in the database. Fifty samples in fields were taken to make an N-fertilizer dosage map. Mean absolute error of these data was 0.59. The Kring method was used to interpolate data between sampling nodes. The interpolated data was used to make a soil OMC map. Also an N-fertilizer dosage map was drawn using the soil OMC map. The N-fertilizer dosage was determined by the fertilizing equation recommended by National Institute of Agricultural Science and Technology in Korea. Use of the N-fertilizer dosage map would increase precision fertilization up to 91% compared with conventional fertilization. Therefore, the developed electronic mapping system was feasible to not only precision determination of N-fertilizer dosage, but also reduction of environmental pollution.

Digital mapping of soil carbon stock in Jeolla province using cubist model

  • Park, Seong-Jin;Lee, Chul-Woo;Kim, Seong-Heon;Oh, Taek-Keun
    • 농업과학연구
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    • 제47권4호
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    • pp.1097-1107
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    • 2020
  • Assessment of soil carbon stock is essential for climate change mitigation and soil fertility. The digital soil mapping (DSM) is well known as a general technique to estimate the soil carbon stocks and upgrade previous soil maps. The aim of this study is to calculate the soil carbon stock in the top soil layer (0 to 30 cm) in Jeolla Province of South Korea using the DSM technique. To predict spatial carbon stock, we used Cubist, which a data-mining algorithm model base on tree regression. Soil samples (130 in total) were collected from three depths (0 to 10 cm, 10 to 20 cm, 20 to 30 cm) considering spatial distribution in Jeolla Province. These data were randomly divided into two sets for model calibration (70%) and validation (30%). The results showed that clay content, topographic wetness index (TWI), and digital elevation model (DEM) were the most important environmental covariate predictors of soil carbon stock. The predicted average soil carbon density was 3.88 kg·m-2. The R2 value representing the model's performance was 0.6, which was relatively high compared to a previous study. The total soil carbon stocks at a depth of 0 to 30 cm in Jeolla Province were estimated to be about 81 megatons.

사영에 의한 반무한지반의 비선형해석 (A Method for Nonlinear Dynamic Response Analysis of Semi-infinite Foundation Using Mapping)

  • 이춘길
    • 한국지반공학회논문집
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    • 제22권4호
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    • pp.5-10
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    • 2006
  • 반무한 영역을 유한영역에 사영한 다음 반무한지반의 비선형동적응답해석에 대한 특수한 유한 차분법을 제안하였다. 해석대상의 주요 부분은 동일 길이로 하고, 주변은 축소, 사영함으로서 무한영역을 유한영역으로 변환 후 차분하였다. 우선 반무한 지반의 선형모델의 응답으로서 계산값과 이론값의 결과를 비교하였다. 선형모델에 대한 제안법의 계산결과는 Lamb의 해석결과와 양호하게 일치했다. 또 간단한 모델에 의한 선형, 비선형해석도 소규모 mesh에 의한 응답결과와 대규모 mesh에 의한 응답결과는 일치하고 제안법의 유효성을 나타내었다.

폐광산의 토양오염영역 및 폐기된 광미의 탐지 (Geophysical Applications on the Soil-contamination Mapping and Detection of Buried Mine Tailings in the Abandoned Mine Area)

  • 이상규;황세호;이태섭
    • 자원환경지질
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    • 제30권4호
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    • pp.371-377
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    • 1997
  • This paper presents the geophysical applications to the environmenml problem in an abandoned mine area. We would like to focus our attention on the mapping of the soil contamination and the detection of the buried mine tailings. For mapping the soil contamination. measurements of both in-situ magnetic susceptibility (k) and terrain conductivity were carried out. In-situ magnetic susceptibilities of the contaminated soil due to the acid mine drainage show higher values than those of the uncontaminated area. However. those data do not show the correlation with the degree of the soil contamination observed on the surface. The least-squares fitted formula obtained with the measured insitu magnetic susceptibilities is $k=4.8207{\times}W^{0.6332}$, where W is the $Fe^{+2}$ weight percentage. This weight gives most effect to magnetic susceptibility of the soil. Lateral variations of the soil contamination in the shallow subsurface can be detected by the electrical conductivity distributions from EM induction survey. TDIP (Time Domain Induced Polarization) and EM induction surveys were conducted to detect the buried mine tailings. From the results of TDIP, the spatial zone, which shows high chargeability-low resistivity, is interpreted as the buried mine tailings. Therefore, it is concluded that it is possible to discriminate the spatial zone from the uncontaminated ground.

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농경지(農耕地)의 기반조성(基盤造成)을 위한 작도단위(作圖單位) 및 배계(培界)의 기하학적(幾何學的) 형태(形態)에 관한 조사(調査) (A Study on the Geometrical Features of Soil Doundaries and Mapping Units for Consolidation Works of Arable Land)

  • 윤을수;정연태;김정곤;손일수
    • 한국토양비료학회지
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    • 제22권1호
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    • pp.6-11
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    • 1989
  • 우리 나라 농경지토양(農耕地土壤) 작도단위(作圖單位)의 기하학적(幾何學的) 특성(特性)을 조사(調査)하여 농경지(農耕地) 기반조성사업(基盤造成事業)에 필요(必要)한 기초자료(基礎資料)를 얻고자 우리 나라 정밀토양도(精密土壤圖)(축척((縮尺) 1 : 25,000)의 지형별(地形別) 대표토양(代表土壤) 70개(個) 토양통(土壤統)(565개작도단위(個作圖單位))을 중심(中心)으로 Picture Analysis System을 이용(利用)해 작도단위(作圖單位) 특성별(特性別) 크기와 복잡성정도(復雜性程度)를 조사(調査)한 결과(結果)는 다음과 같았다. 1. 조사(調査)한 작도단위(作圖單位)의 평균(平均)크기는 약(約) 22.0ha, 경계선(境界線)길이 2,267m, 장축장(長軸長) 911m 단축장(短軸長) 76m, 도형도(圖形度) 0.104, 예각수(銳角數) 3.5개(個) 이었고, 작도단위(作圖單位)의 복잡성정도(復雜性程度)를 표시(表示)하는 수단(手段)으로서 "단순성지수(單純性指數)" (Simplicity index of mapping unit)를 제시(提示)하였다. 2. 지형별(地形別) 작도단위(作圖單位)의 크기는 하성평탄지(河成平坦地)에 분포(分布)된 것이 43.7ha로 가장 크고 그 다음은 하해혼성평탄지(河海混成平坦地) 40.4ha, 홍적대지(洪積臺地) 22.3ha, 구릉지(丘陵地) 13.8ha, 선상지(扇狀地) 12.5ha, 산록경사지(山麓傾斜地) 9.0ha 등(等)의 순(順)이었고, 곡간지(谷間地)에 분포(分布)된 것이 8.7ha로 가장 작았으며 단순성지수(單純性指數)는 하성평탄지(河成平坦地)에 분포(分布)된 것이 0.44로서 가장 높았고, 하해혼성(河海混成) 평탄지(平坦地) 0.30, 대지(臺地) 및 선상지(扇狀地) 0.24, 구릉지(丘陵地) 0.20, 곡간지(谷間地) 0.15 그리고 산록경사지(山麓傾斜地) 0.13의 순(順)으로 낮아져 지형(地形)이 복잡(復雜)해짐을 나타낼 수 있었다. 3. 토성(土性) 및 경사도(傾斜度) 또는 배수등급별(排水等級別) 작도단위(作圖單位)의 크기는 평탄지(平坦地)에 분포(分布)된 배수약간불량(排水若干不良)한 미사질토(微砂質土)가 46.1~34.1ha로 크면서 단순성지수(單純性指數)도 0.36~0.27 로서 큰 반면, 경사도(傾斜度)가 높아지거나 상대적(相對的)으로 배수양호(排水良好)할수록 그리고 식양질토(埴壤質土) 및 사양질토(砂壤質土)가 면적(面積)도 작고 단순성지수(單純性指數)도 낮아지는 경향(傾向)이었다. 4. 최근(最近) 경지정리(耕地整理) 실시지구(實施地區)에서 농구(農區)의 크기와 단순성지수(單純性指數)와의 관계(關係)는 정상관(正相關)($r=0.8057^{**}$)이 있었고 차후(次後) 경지정리등(耕地整理等) 농경지(農耕地) 기반(基盤) 조성시(造成時)는 협업화영농관리(協業化營農管理) 및 공동기계화(共同機械化) 작업(作業) 등(等)을 위하여 작도단위(作圖單位)의 형태적(形態的) 특성(特性)을 기초(基礎)로 설계(設計)하고 농구(農區)의 경계(境界)를 가능(可能)한 작도단위(作圖單位)의 경계선(境界線)과 일치(一致)하도록 고려(考慮)할 필요성(必要性)이 있었다.

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Mapping of Quantitative Trait Loci for Yield and Grade Related Traits in Peanut (Arachis hypogaea L.) Using High-Resolution SNP Markers

  • Liang, Yuya;Baring, Michael R.;Septiningsih, Endang M.
    • Plant Breeding and Biotechnology
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    • 제6권4호
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    • pp.454-462
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    • 2018
  • Yield and grade are the key factors that affect production value of peanut. The objective of this study was to identify QTLs for pod yield, hundred-seed weight, and total sound mature kernel (TSMK). A total of 90 recombinant inbred lines, derived from Tamrun OL07 and a breeding line Tx964117, were used as a mapping population and planted in Brownfield and Stephenville, Texas. A genetic map was developed using 1,211 SNP markers based on double digest restriction-site associated DNA sequencing (ddRAD-seq). A total of 10 QTLs were identified above the permutation threshold, three for yield, three for hundred-seed weight and four for TSMK, with LOD score values of 3.7 - 6.9 and phenotypic variance explained of 12.2% - 35.9%. Among those, there were several QTLs that were detected in more than one field experiment. The commonly detected QTLs in this study may be used as potential targets for future breeding program to incorporate yield and grade related traits through molecular breeding.

Spatial Pedological Mapping Using a Portable X-Ray Fluorescence Spectrometer at the Tallavera Grove Vineyard, Hunter Valley

  • Jang, Ho-Jun;Minasny, Budiman;Stockmann, Uta;Malone, Brendan
    • 한국토양비료학회지
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    • 제49권6호
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    • pp.635-643
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    • 2016
  • Wine consumers desire to drink a high quality wine. For producing high quality wine, high quality soil is required. Conventionally, soil quality is assessed qualitatively. Using traditional laboratory methods, quantitative data can be obtained for management purpose, but it is time consuming and expensive. Therefore, new technology aims to address these limitations, namely portable X-Ray fluorescence spectrometers (pXRF). This instrument can be used directly in the field, requires no soil sample preparations, and can simultaneously measure a wide range of elements qualitatively that are useful for pedological studies. The chemical composition (Ca, Fe, Ti and Zr) of soils at Tallavera Grove vineyard in New South Wales, Australia, was studied using a pXRF. The analysis of the soil's elemental concentration (i.e. Ca and Fe) using pXRF supports management decisions. Measuring the soil's Ca concentration can be used to identify Ca-rich parent materials (limestone). The limestone indicates good soil conditions for vine production. Fe content was used to identify areas of texture-contrast soils or soil with accumulation of clays in the B horizon. In addition, a soil weathering index was calculated using elemental concentrations (i.e. Ti and Zr) to explore the history of soil formation for making decision of management. This index showed that the soil in the vineyard was affected by two processes: the deposition of materials from elsewhere (Aeolian transport or soil erosion) and mixing of materials from upslope.

Estimation of spatial parameters to be included in 3D mapping for long-term forest road management

  • Choi, Sung-Min;Kweon, Hyeongkeun;Lee, Joon-Woo
    • 농업과학연구
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    • 제47권4호
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    • pp.727-742
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    • 2020
  • Point cloud-based 3D maps can obtain many kinds of information for maintenance work on forest road networks. This study was conducted to compare the importance of each factor to select the factors required for the mapping of 3D forest road maps. This can be used as basic data for attribute information required to maintain forest road networks. The results of this study found that out of a total of 30 indexes extracted for mapping 3D forest roads, a total of 21 indexes related to stakeholder groups were significantly different. The importance of the index required by the civil service group was significantly higher than that of the other groups overall. In the case of the academic group, the index importance for cut slope, fill slope, and drainage facility was significantly higher. On the other hand, the index importance for the forestry cooperative and forest professional engineer group was mostly distributed between the civil servants' group and the academic group. In particular, the type of drainage system showed the highest value among the detailed indexes. Overall, drainage related factors in this survey had high coefficient values. The impact of water on forest roads was the most important part in road maintenance. In addition, the soil texture had a high value in relation to slope stability. This is thought to be because the texture of the soil affects the stability of the slope.