• 제목/요약/키워드: Soil moisture level

검색결과 252건 처리시간 0.035초

골프장에서 지렁이 분변토 발생의 계절적 변화 (Seasonal Earthworm Casting Activity on Korean Golf Courses)

  • 신종창;김종경;홍용;김영섭;김진호;박대섭;이동운
    • Weed & Turfgrass Science
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    • 제4권4호
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    • pp.368-375
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    • 2015
  • 골프장 잔디위로 배출되는 지렁이 분변토는 잔디관리와 경기진행에 있어 피해를 주고 있다. 본 연구는 골프장에서 지렁이 분변토의 발생변화를 시기별, 지역별(경기도 가평, 군포, 안성, 용인, 부산 금정)로 조사하였으며 분변토 발생량이 많은 지역과 없는 지역을 구분하여 토양 수분과 토양온도 및 지렁이 개체수를 조사하였다. 지렁이 분변토는 4월부터 11월까지 년 중 골프장 잔디에 발생하고 있었으며 골프장 별 및 시기별에 따라 차이가 있었다. 동일골프장에서 조사 지역에 따라 차이를 보였다. 분변토 발생량과 지렁이 수는 양의 상관관계가 있었으며 분변토 발생이 많은 지역과 없는 지역간의 토양 온도는 차이가 없었으나 토양수분은 분변토 수가 많은 지역에서 높았다. 지렁이 분변토는 토양온도 $2.1^{\circ}C$에서 $33.1^{\circ}C$의 범위에서 확인되었는데 주로 $10-15^{\circ}C$ 사이에 발생하였다. 또한 토양수분은 4.9-44.1% 범위 내에서 발생하였는데 주로 25% 내외에서 발생량이 많았다.

Analysis of Paddy Soil Chemical Properties and Rice Quality in Central Area (Sejong) in Korea

  • Choi, Nag-Gor;Park, Jong-Hyun;Kang, Seong-Soo
    • 한국토양비료학회지
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    • 제51권1호
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    • pp.61-70
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    • 2018
  • This study was carried out to review and compare crop cultivations upon chemical properties of paddy soil and qualitative characteristics of rice in Sejong-city from a point of view of farming extension to rice farmers and to utilize the result of the study as a basic guideline for precise agricultural practice. The pH in soils of Sejong was about 6.1-6.6 and had no difference with an average pH of paddy soils in Chung-Nam with pH 6.1. However, the average of organic matter, calcium (Ca) and available silicate in Sejong was lower than the average of them in Chung-Nam. The yields of rice were higher in 2010 than in 2011 and 2012, and the protein contents of rice were the highest in 2011 while the lowest water contents of rice in 2011. The protein contents upon regions were the highest in 2011 with 6.1%, and the amylose contents were the highest in Yeondong-myun, Jeoneu-myun, and Yeonseo-myun in 2010 while Kumnam-myun and Jeondong-myun were the highest in 2012. With the increase of precipitation, the protein content level in rice was increased while the amylose content level tended to decrease. Correlations between the chemical properties of paddy soil and the quality of rice and between level of organic matter in soil and amylose contents were negative (r = -0.507), and the correlation between the moisture contents and amylose contents (r = 0.419) and between the water contents and whiteness (r = 0.485) were positive. Because the quantity and quality of rice yield is determined by the soil characteristics, the consultation to farmers for the proactive soil analysis and for the maintenance of stable level of pH, organic matter and available silicate based on historical results of analysis is highly recommended. Also, the analysis on the effect of the weather and the soil characteristics affecting the quality and quantity of rice would be another good way.

Hydrological Variability of Lake Chad using Satellite Gravimetry, Altimetry and Global Hydrological Models

  • Buma, Willibroad Gabila;Seo, Jae Young;Lee, Sang-IL
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2015년도 학술발표회
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    • pp.467-467
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    • 2015
  • Sustainable water resource management requires the assessment of hydrological variability in response to climate fluctuations and anthropogenic activities. Determining quantitative estimates of water balance and total basin discharge are of utmost importance to understand the variations within a basin. Hard-to-reach areas with few infrastructures, coupled with lengthy administrative procedures makes in-situ data collection and water management processes very difficult and unreliable. In this study, the hydrological behavior of Lake Chad whose extent, extreme climatic and environmental conditions make it difficult to collect field observations was examined. During a 10 year period [January 2003 to December 2013], dataset from space-borne and global hydrological models observations were analyzed. Terrestial water storage (TWS) data retrieved from Gravity Recovery and Climate Experiment (GRACE), lake level variations from Satellite altimetry, water fluxes and soil moisture from Global Land Data Assimilation System (GLDAS) were used for this study. Furthermore, we combined altimetry lake volume with TWS over the lake drainage basin to estimate groundwater and soil moisture variations. This will be validated with groundwater estimates from WaterGAP Global Hydrology Model (WGHM) outputs. TWS showed similar variation patterns Lake water level as expected. The TWS in the basin area is governed by the lake's surface water. As expected, rainfall from GLDAS precedes GRACE TWS with a phase lag of about 1 month. Estimates of groundwater and soil moisture content volume changes derived by combining altimetric Lake Volume with TWS over the drainage basin are ongoing. Results obtained shall be compared with WaterGap Hydrology Model (WGHM) groundwater estimate outputs.

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Climate Change Impacts in Natural Resources and Livestock in Mongolia Climate

  • Batima, P.;Natsagdorj, L.;Bayarbaatar, L..;Bolortsetseg, B.;Natsagsuren, N.;Erdenetsetseg, B.
    • 한국제4기학회지
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    • 제18권2호통권23호
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    • pp.103-104
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    • 2004
  • This paper discuss some results of observed changes of meteorological elements as temperature, precipitation and some extreme indexes in Mongolia. Mongolia is one of the largest landlocked countries in the world. The climate is characterized by a long lasting cold winter, dry and hot summer, low precipitation, high temperature fluctuation and relatively high number of sunny days per year. During last 60 years the annual mean air temperature has risen $1.66^{\circ}C$. Intensive warming of > $2^{\circ}C$ was observed at higher altitudes of high mountains when warming of < $1^{\circ}C$ was observed the Domod steppe and the Gobi Desert. Heat Wave Duration have statistically significant risen trend with increaded number of days by 8-18 at significance level of 95-99.9% depending on geography and Cold Wave Duration have shortened by 13.3 days significance level of 95-99%. In general, by the amount of precipitation, Mongolia falls in semi-arid and arid region. It is 300-350 mm in the high mountain regions while it is only 50-150 mm in Gobi Desert regions. The changes of annual precipitation have very localized character i.e.decreasing at one site and increasing at a sit nearby. Annual precipitation decreased by 30-90 mm in the northern-central region and increased by 2-60 mm in the western and eastern region. The magnitude of alteration changes in precipitation regardless increasing or decreasing is 5-25%. A trends, significant at the level of 90%, found where changes are more than 40 mm or more than 15% of annual mean value. Moreover, the soil moisture resources was decreased in the last 40 years. Specially, moisture contents of the top soil have decreased 2 times(N. Natsagsuren, 2002). Months of June and July in Mongolia is the year that moisture is not inhibiting vegetation growth. Unfortunately, its also found that moisture in this time tends to decrease. Increased temperature, decreased precipitation and soil moisture are most likely resulted in occurences of more intense drought spells that have taken place during the recent years. Intimately, these changes have considerable impact on livestock in Mongolia.

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포장용수량과 포화 반죽 토양용액의 전기전도도 비교 (The Comparison of Electrical Conductivity for Soil Solutions Extracted in Field Capacity and Saturation-Paste)

  • 이예진;이종식;양재의
    • 한국토양비료학회지
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    • 제43권6호
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    • pp.776-781
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    • 2010
  • 본 실험은 토양의 염류도 평가를 위한 전기전도도 측정시 기준으로 적용되는 포화 전기전도도가 이상적인 측정방법인 포장용수량의 전기전도도를 대표할 수 있는지 평가하기 위하여 수행되었다. 염류집적 시설재배지 22점과 간척지 토양 18점을 채취하여 포화반죽과 포장용수량의 토양용액을 추출하고, 주요 구성 양이온, 음이온과 전기전도도를 비교하였다. 시설재배지 토양의 양이온, 음이온과 간척지 토양에서 ${NO_3}^-$${PO_4}^{3-}$를 제외한 나머지 양이온, 음이온 모두 높은 상관을 나타내었고, 포장용수량과 포화 전기전도도 또한 높은 상관관계를 보였다. 포화 전기전도도와 불포화 조건인 포장용수량 전기전도도를 비교하였을 때 시설재배지 토양에서는 기울기가 0.923, 간척지 토양에서는 1.009로 거의 차이가 없었으며, 통계 결과 유의성이 인정되지 않아 포화반죽으로 전기전도도를 평가하는 것이 합리적인 것으로 판단되었다. 시설재배지와 간척지 토양을 sand, silt, clay 각각을 기준으로 비교한 결과 sand 함량과 포장용수량, 포화 전기전도도 비율이 비례하는 것으로 나타났다. 시설재배지 토양에서 sand 50% 이하에서는 0.811, Sand 50% 이상에서는 1.179, 간척지 토양은 sand 50% 이하에서 0.848, Sand 50% 이상에서 1.087배 차이나는 것으로 나타났으며, sand 함량이 많을수록 포장용수량과 포화 수분퍼센트의 차이가 크게 나타나 토성에 의한 수분 보유력이 관련된 것으로 판단되었다.

Spatial Estimation of soil roughness and moisture from Sentinel-1 backscatter over Yanco sites: Artificial Neural Network, and Fractal

  • Lee, Ju Hyoung
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2020년도 학술발표회
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    • pp.125-125
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    • 2020
  • European Space Agency's Sentinel-1 has an improved spatial and temporal resolution, as compared to previous satellite data such as Envisat Advanced SAR (ASAR) or Advanced Scatterometer (ASCAT). Thus, the assumption used for low-resolution retrieval algorithms used by ENVISAT ASAR or ASCAT is not applicable to Sentinel-1, because a higher degree of land surface heterogeneity should be considered for retrieval. The assumption of homogeneity over land surface is not valid any more. In this study, considering that soil roughness is one of the key parameters sensitive to soil moisture retrievals, various approaches are discussed. First, soil roughness is spatially inverted from Sentinel-1 backscattering over Yanco sites in Australia. Based upon this, Artificial Neural Networks data (feedforward multiplayer perception, MLP, Levenberg-Marquadt algorithm) are compared with Fractal approach (brownian fractal, Hurst exponent of 0.5). When using ANNs, training data are achieved from theoretical forward scattering models, Integral Equation Model (IEM). and Sentinel-1 measurements. The network is trained by 20 neurons and one hidden layer, and one input layer. On the other hand, fractal surface roughness is generated by fitting 1D power spectrum model with roughness spectra. Fractal roughness profile is produced by a stochastic process describing probability between two points, and Hurst exponent, as well as rms heights (a standard deviation of surface height). Main interest of this study is to estimate a spatial variability of roughness without the need of local measurements. This non-local approach is significant, because we operationally have to be independent from local stations, due to its few spatial coverage at the global level. More fundamentally, SAR roughness is much different from local measurements, Remote sensing data are influenced by incidence angle, large scale topography, or a mixing regime of sensors, although probe deployed in the field indicate point data. Finally, demerit and merit of these approaches will be discussed.

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입지환경인자를 바탕으로 한 편백의 지위지수 추정에 관한 연구 (The Effects of Site Environmental Factors on Estimation of Site Index Function for Chamaecyparis obtusa Endlicher Stands)

  • 김대현;김의경;이성기;정영교;정진현
    • 한국환경과학회지
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    • 제17권8호
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    • pp.891-898
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    • 2008
  • This study was conducted to develop the effects of site environmental factors on estimation of site index function for Chamaecyparis obtusa Endlicher stands. We derived nonlinear growth equation and the draw site index curves by applying this estimated equation. This study with Chapman-Richards function showed significant P-value which was less then 0.0001 and $R^2$ value 0.5947. This study was conducted to develop the feasible site index equation of Chamaecyparis obtusa Endlicher. For the table, the data of 82 sample areas that were thought to be without errors among the data of Chamaecyparis obtusa Endlicher sample area located on the value-oriented forest location chart were used and estimated. After analyzing the quantification method I based on 13 environmental factors to develop the score table for the site-index estimation of Chamaecyparis obtusa Endlicher, $R^2$ value of the model was 0.7555. It has been analyzed that the scope value of Soil moisture in horizon A was 7.5045, that of total soil depth was 6.3896, that of topography was 5.3471, that of slope was 4.7000 and that of aspect was 3.2038. After analyzing the partial correlation to examine the factors that affected most the site-index of Chamaecyparis obtusa Endlicher, it has been noted that the partial correlation of climatic zone was 0.4987, which was highest, and it was followed by Soil moisture in horizon A (0.4592), slope (0.4537), topography (0.3299) and total soil depth (0.1035). As a result of conducting the significance test for partial correlation, it has been found that topography, climatic zone, parent rock, slope, altitude, aspect, Soil moisture in horizon A, soil hardness in horizon A and total soil depth were recognized significant with 1% of significance level and sedimentary type and soil texture in horizon A were recognized significant with 5% of significance level.

Altitudinal Variation in Species Composition and Soil Properties of Banj Oak and Chir Pine Dominated Forests

  • Kumar, Munesh;Singh, Harpal;Bhat, Jahangeer A.;Rajwar, G.S.
    • Journal of Forest and Environmental Science
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    • 제29권1호
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    • pp.29-37
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    • 2013
  • The study was carried out in two different forest types viz., Banj oak and Chir pine forests to assess the variation in forest species composition and soil properties along altitudinal gradients in the Garhwal Himalayas. The results of the study showed that between the forests soil moisture was higher in Banj oak forest because of closed canopy and dense forest compared to Chir pine forest. The sand particles were reported higher in Banj oak forest which might be due to the addition of organic matter favouring coarse structure of soil, helping in holding maximum water in soils. However in the Chir pine forest low amount of soil organic matter and presence of clayey soil, develops soil compactness which reduces the penetration of water resulting in high soil bulk density. The higher accumulation of litter and presence of moisture in Banj oak forest favours higher nutrient level of nitrogen, phosphorus and potassium compared to Chir pine forest. The soil organic carbon also reduced with increasing altitude at both gradients. While bulk density has reverse trend with soil organic carbon in both the forests at different peaks of same region. In Banj oak forest, the highest density and total basal cover was reported 1,100 tree $ha^{-1}$ and 58.86 $m^2\;ha^{-1}$ respectively. However, the highest values of density and total basal cover of Chir pine forest was 560 tree$ha^{-1}$ and 56.94 $m^2\;ha^{-1}$ respectively. The total density and basal cover of both the forests reduced with increasing altitude. The study concludes that Banj oak forest has better nutrient cycling ability, well developed foest floor and has a greater protective and productive features compared to the Chir pine forest which is without lower vegetation cover and having only pine litter accumulation which does not allow any other species to grow.

강원도지역의 토양동결심 및 상록식물의 함수량 추이에 관한연구 (1) (Studies on the soil freezing depth and change of moisture contents in evergreen plants upon subzero temperature in)

  • 홍종운;허범양;원경열;임병춘;이기철;하상건
    • 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.

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육묘용 로봇이식기 그리퍼의 개발 및 이식 성능 평가 (Development of a Gripper for Robotic Transplanter and Evaluation of Its Transplanting Performance)

  • 류관희;김기영;박정인
    • Journal of Biosystems Engineering
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    • 제23권3호
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    • pp.271-276
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    • 1998
  • A gripper mechanical design using a pneumatic system was developed to successfully grip, hold, and release a seedling plug for transplanting it. The gripper comprised of two air cylinders and shovel-type fingers. The gripper can grasp and hold a seedling by sliding the two fingers attached to the two separate air-cylinders, mounted at an angle of 15$^{\circ}$ When releasing a plug, retraction of the fingers gives a seedling little attachment to the gripper. To prevent seedling from attaching to the fingers, press-plates were attached to the end of the gipper. Transplanting performance of the developed gripper was tested with cucumber seedlings at different soil moisture contents. Overall transplanting performance of developed gipper was higher than the performance of the previously developed gripper. Best transplanting result was achieved at medium level of soil moisture content.

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