• 제목/요약/키워드: Soil Water

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토양수분퍼텐셜이 복분자 습해와 토양특성에 미치는 영향 (Effects of Soil Water Potential on the Moisture Injury of Rubus coreanus Miq. and Soil Properties)

  • 안병구;김갑철;김대향;이진호
    • 한국토양비료학회지
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    • 제44권2호
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    • pp.168-175
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    • 2011
  • 토양수분포텐셜이 복분자 생육에 미치는 영향을 조사하기 위하여 복분자 시설하우스에서 -5 ~ -40 kPa 수준으로 토양수분을 처리하였다. 시설하우스내의 토양유효수분은 5.6%이었고, 수분포텐셜에 따라 토양수분함량이 높아지면 토양 pH와 치환성 Ca은 증가하였고, 치환성 K와 전질소 함량은 감소하였으며, 유기물함량은 수분처리 9일 이후부터 감소하였다. 수분포텐셜과 토양수분함량 간에는 y = 96.534 - 20.28In(x)의 지수함수 근사식이 성립되었다. 수분포텐셜이 -20 kPa (토양 수분 27.5%) 이상이면 복분자 잎의 엽록소 함량이 감소하였고 질소흡수가 억제되며, P 함량은 수분공급 시간에 따라 증가하였다. 수분포텐셜 -20 kPa 이상의 수준으로 7일 이상이 경과하면 뿌리활력이 급격히 감소되어 생육이 위축되었다. 지상부에 대한 뿌리비율 (T/R률)은 수분공급 9일까지 급격히 감소하였다. 휴면기의 복분자 줄기와 뿌리의 탄수화물 함량은 -5 kPa과 -10 kPa 처리구에서 가장 낮아 동해 위험도가 가장 높았다.

수질오염총량관리 단위유역내 토양 양분 및 수질오염 부하량 상관관계 비교 (Correlation between Soil Nutrient Contents and Water Pollutant Loads in Hydrologic Unit Watersheds: Implication on the Total Maximum Daily Loads (TMDLs))

  • 조경식;이호식
    • 한국물환경학회지
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    • 제27권4호
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    • pp.509-515
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    • 2011
  • For this study the 4 sub-watersheds Okdong A, Hankang B, Jecheon A and Hankang C which are the main streams of the Han River within the mid-level region of Chungju Dam are selected and the analysis of soils has been carried out through the soil basic survey. When it comes to the soil erosion amount the soil nutrient load has been calculated by utilizing the RUSLE erosion equation. In case of the data related to the measurement of water flow and quality the information available from the "Water Information System" one of the websites run by the Ministry of Environment has been used to calculate the water pollution load. The correlation between the soil nutrient load and the water pollutant load has been analyzed through making comparison. According to the results related to the soil nutrient load of each sub-watershed the Hankang C shows the highest values TOC 29,986.92 ton/yr, TN 3,860.33 ton/yr and TP 973.97 ton/yr respectively. Even when it comes to the loads related to water quality the Hankang C shows also comparatively high values TOC 6,625.64 ton/yr, TN 7,335.01 ton/yrand TP 145.49 ton/yr respectively. The soil nutrient loads of the sub-watersheds are shown to increase towards the lower stream meaning the load increases in the order of Hankang CHankang B and Okdong A. When it comes to the water pollutant load the value goes up along down the water system meaning the load gets higher in the order of Hankang C, Hankang B and Okdong A while utilizing the mainstream within the mid-level region of Chungju Dam as the basis. The correlation study showed that the nutrient content of soil is proportional to the pollutant load in water with the strongest positive correlation with TOC.

Simultaneous Determination of 4-Nitrotoluene and Benzophenone in Ground Water and Soil by Gas Chromatography-Mass Spectroscopy

  • Kwon, Oh-Seung;Kim, Eun-Young;Ryu, Jae-Chun
    • 분석과학
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    • 제16권1호
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    • pp.59-69
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    • 2003
  • Benzophenone (BZP) and 4-nitrotoluene (4-NT) listed as endocrine disrupting chemicals are suspected to contaminate ground water sites and soil. Analytical method for simultaneous determination of the two chemicals in soil and ground water was developed by gas chromatography-mass spectrometry. Water (100 ml) was extracted with hexane, and soil (10 g) was extracted with methanol and hexane. Recovery in water was >72% for BZP and 90-118% for 4-NT. Recovery for 4-NT and BZP in soil was 51-59% with coefficient variation of less than 19.5%. Calibration curves showed a good linearity with $r^2=0.997$. In water and soil collected at nation-wide sites, BZP was found at 5 sites among 43 water sites at the concentration of $14.87{\pm}3.83ng/100 ml$. No 4-NT was found. It is suggested that this method is appropriate to the simultaneous quantitation of 4-NT and BZP in ground water and soil samples.

Soil Water Monitoring in Below-Ground Ectomycorrhizal Colony of Tricholoma Matsutake

  • Koo, Chang-Duck;Kim, Je-Su;Lee, Sang-Hee;Park, Jae-In;Kwang- Tae Ahn
    • 한국제4기학회지
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    • 제17권2호
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    • pp.129-133
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    • 2003
  • Water is critically important for Tricholoma matsutake(Tm) growth because it is the major component of the mushroom by over 90%. The mushroom absorbs water through the below ground hyphal colony. Therefore, the objectives of our study were to investigate spatio-temporal water changes in Tm colonies. This study was carried out at Tm fruiting sites in Sogni Mt National Park, where the below-ground mushroom colonies have been irrigated. To identify spatial water status within the Tm soil colony soil moisture and ergosterol content were measured at six positions including a mushroom fruiting position on the line of the colony radius. To investigate temporal soil moisture changes in the soil colony, Time Domain Reflectometry(TDR) sensors were established at the non-colony and colony front edge, and water data were recorded with CR10X data logger from late August to late October. Before irrigation, whereas it was 12.8% at non-colony, the soil water content within Tm colony was 8.0% at 0-5cm from the colony front edge, 6.2% at 10-15cm and 6.5-7.5% at 20-40cm. And the content was 12.1% at 80cm distance from the colony edge, which is similar to that at the non-colony. In contrast, ergosterol content which is proportional to the live hyphal biomass was only 0.4${\mu}g$/g fresh soil at the uncolonized soil, while 4.9 $\mu\textrm{g}$/g fresh soil at the front edge where the hyphae actively grow, and 3.8 ${\mu}g$/g fresh soil at the fruiting position, l.1${\mu}g$/g at 20cm distance and 0.4${\mu}g$/g in the 40cm rear area. Generally, in the Tm fungal colony the water content changes were reversed to the ergosterol content changes. While the site was watered during August to October, the soil water contents were 13.5∼23.0% within the fungal colony, whereas it was 14.5∼26.0% at the non-colony. That is, soil water content in the colony was lower by 1.0∼3.0% than that in the non-colonized soil. Our results show that Tm colony consumes more soil water than other parts. Especially the front 30cm within the hyphal colony parts is more critical for soil water absorption.

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Growth and yield responses of rice varieties to various soil water deficit conditions under different soil types

  • Kikuta, Mayumi;Samejima, Hiroaki;Magoti, Rahab;Kimani, John M.;Yamauchi, Akira;Makihara, Daigo
    • 한국작물학회:학술대회논문집
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    • 한국작물학회 2017년도 9th Asian Crop Science Association conference
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    • pp.322-322
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    • 2017
  • To avoid drought stress under rainfed upland conditions, it is important for rice to efficiently utilize water at shallow soil layers supplied by rainfall, and access to water retained in deer soil layers. The root developmental characteristics of rice, which play important role in the adaptability to drought conditions, vary depending on the variety. Moreover, water availability for plant differs depending on the soil types that have different physical properties such as water holding capacity, permeability, capillary force, penetration resistance, etc. In this study, we evaluated growth and yield responses of rice varieties to various soil water deficit conditions under three different soil types. The experiment was conducted in a plastic greenhouse at the Kenya Agricultural and Livestock Research Organization-Mwea from October 2016 to January 2017. Two upland varieties (NERICA 1 and 4) and one lowland variety (Komboka) were grown in handmade PVC pots (15.2 cm diameter and 85.0 cm height) filled with three different types of soil collected from major rice-growing areas of the country, namely black cotton (BC), red clay (RC), and sandy clay (SC). Three watering methods, 1) supplying water only from the soil surface (W1), 2) supplying water only from the bottom of the pots (W2), and 3) supplying water both from the soil surface and the bottom of pots (W3), were imposed from 40 days after sowing to maturity. Soil water content (SWC) at 20, 40, and 60 cm depths was measured regularly. At the harvesting stage, aboveground and root samples were collected to determine total dry weight (TDW), grain yield, and root length at 0-20, 20-40, 40-60, and 60-80 cm soil layers. Irrespective of the watering methods, the greatest root development was obtained in RC, while that in BC was less than other two soils. In BC, the degree of yield reduction under W1 was less than that in RC and SC, which could be attributed to the higher water holding capacity of BC. In RC, the growth and yield reduction observed in all varieties under W1 was attributed to the severe drought stress. On the other hand, under W2, SWC at the shallow soil depth in RC was maintained because of its higher capillary force compared with BC and SC. As the result, growths and yields in RC were not suppressed under W2. In SC, deep root development was not promoted by W2 irrespective of the varieties, which resulted in significant yield losses. Under W1, the rice growth and yield in SC was decreased although shallow root development was enhanced, and the stomatal conductance was maintained higher than RC. It was suspected that W1 caused nutrients leaching in SC because of its higher permeability. Under rainfed conditions, growth and yield of rice can be strongly affected by soil types because dynamics of soil water conditions change according to soil physical properties.

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가축분뇨 액비 살포가 새만금유역에서의 논토양과 수질에 미치는 영향 (Effect of Livestock Liquid Manure Released at a Rice Field on Quality of Soil and Water in the Saemangeum Watershed)

  • 김미숙;곽동희
    • 상하수도학회지
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    • 제30권1호
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    • pp.19-31
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    • 2016
  • The Saemangeum watershed is required to manage water pollution effectively but the effect of liquid manure (LM) on soil and water quality in the basin is not clearly identified as yet. This study aims at assessing the effect on soil of a rice field and water quality of water bodies near the rice field during rice-crop time period to find out the effect of LM, the effect of rainfall, and the effect of rice-crop environment on soil and water quality by analyzing data of nitrogen components. As a result of the LM distribution, $NO_3-N$ was much higher than other N components in the entire soil layers and it was accelerated by rainfall right after the LM distribution. Compared to chemical fertilizer (CF), LM was slightly affected but still influenced on the surface water quality. During weak rainfall, low nitrogen concentration in topsoil was resulted as NH3-N decreased and Org-N and $NO_3-N$ increased. $NO_3-N$ concentration in the water of irrigation canals increased with time. During intensive rainfall, $NO_3-N$ and Org-N of the soil were measured highly in the submerged condition, while the water quality of the rice field was lower due to flooding into the irrigation canal as well as the growth of the rice plants. Also, total nitrogen was increased more than 7 times and it showed serious water quality deterioration due to LM and excessive fertilizer distribution, and rainfall during all rice-crop processes. The effect of LM on water quality should be studied consistently to provide critical data while considering weather condition, cropping conditions, soil characteristics, and so on.

노지 과수원 토성별 수분보유 특성 및 FDR 센서 보정계수 비교 (Comparisons of Soil Water Retention Characteristics and FDR Sensor Calibration of Field Soils in Korean Orchards)

  • 이기람;김종균;이재범;김종윤
    • 생물환경조절학회지
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    • 제31권4호
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    • pp.401-408
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    • 2022
  • 최근 원예작물의 지속가능한 생산을 위한 작물 생육환경 센싱 기반 복합환경제어시스템 연구와 산업적 이용이 부각되면서, 노지재배에 적용하기 적합한 토양센서 활용 방안 연구가 활발히 이루어지고 있다. 본 연구는 산업 및 연구 현장에서 많이 사용되고 있는 TEROS 12 FDR 센서(frequency domain reflectometry sensor)를 노지 과수원의 토양에 알맞게 활용하기 위하여 국내 세 지역 과수원 토양의 토성별 FDR 센서 활용 방법을 제시하고자 수행하였다. 실제 과수가 재배되고 있는 각 과수원에서 토양을 채취하여, 토성 및 토양수분보유곡선을 조사하였으며, 토양별 TEROS 12 센서 Raw 값과 이에 대응하는 용적수분함량 값을 선형 회귀 분석, 3차 회귀 분석을 통해 보정식을 얻은 뒤 제조사에서 제공하는 광질 토양 보정식과 비교 분석하였다. 채취한 세 과수원의 토양은 모두 토성이 달랐으며, 토성에 따라 각 보수력에 따른 용적수분함량 수치에 차이가 있었다. 또한, TEROS 12 센서 보정식에서는 모든 토양에서 3차 회귀 분석 보정식이 결정계수 0.95 이상으로 가장 높게 나타났으며, RMSE도 가장 낮게 나타났다. 제조사에서 제공하는 보정식을 사용하여 TEROS 12 센서의 용적수분함량을 보정할 경우 토양에 따라 실제 수치에 비해 최대 0.09-0.17m3·m-3가량 낮게 나타나, FDR 센서 사용시 적용 토양에 알맞은 보정이 반드시 선행되어야 함을 확인하였다. 또한 토성에 따라 토양의 보수력 구간에 따른 용적수분함량 범위의 차이가 있었으며, 토양 용적수분함량의 수치 해석에 보수력 정보가 수반되어야 할 것으로 나타났다. 또한, 사질이 많은 토양에서는 관수 개시점 측정을 위해 FDR 센서를 활용하는 데 있어 용적수분함량 측정 범위가 상대적으로 좁아 정밀도가 떨어질 것으로 판단되었다. 결론적으로 토양에서 FDR 센서를 통해 토양수분의 변화를 알맞게 해석하고 노지에서 알맞은 관수 시점을 선정하기 위해서는, 적용 토양의 수분보유특성을 파악하고 FDR 센서 보정을 선행하여 올바른 토양 수분 정보 제공이 필요할 것이다.

북한산국립공원에서 동결융해침식토사 및 유량이 계류수질에 미치는 영향 분석 (Analysis of Influences of the Solifluction Soil and Stream flow on the Stream Water Quality of Bukhansan National Park)

  • 박재현
    • 한국환경복원기술학회지
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    • 제6권2호
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    • pp.11-20
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    • 2003
  • This research was conducted to investigate the influences of the solifluction soil and amount of flow on the stream water quality of the Bukhansan National Park from March to october, 2002. The average pH of stream water was higher than that caused by solifluction soil. The average electrical conductivity of upstream water was about 2.1~2.8 times lower than that of downstream water. Linear regression analysis showed that pH and amount of anion($Cl^-$, ${NO_3}^-$, ${SO_4}^{2-}$) of stream water were very significantly correlated with those at the caused by solifluction soil. Structures for erosion control along both sides of stream channel should be designed in order not to influence upon solifluction soil and stream water quality.

A comparative experimental study on the mechanical properties of cast-in-place and precast concrete-frozen soil interfaces

  • Guo Zheng;Ke Xue;Jian Hu;Mingli Zhang;Desheng Li;Ping Yang;Jun Xie
    • Geomechanics and Engineering
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    • 제36권2호
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    • pp.145-156
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    • 2024
  • The mechanical properties of the concrete-frozen soil interface play a significant role in the stability and service performance of construction projects in cold regions. Current research mainly focuses on the precast concrete-frozen soil interface, with limited consideration for the more realistic cast-in-place concrete-frozen soil interface. The two construction methods result in completely different contact surface morphologies and exhibit significant differences in mechanical properties. Therefore, this study selects silty clay as the research object and conducts direct shear tests on the concrete-frozen soil interface under conditions of initial water content ranging from 12% to 24%, normal stress from 50 kPa to 300 kPa, and freezing temperature of -3℃. The results indicate that (1) both interface shear stress-displacement curves can be divided into three stages: rapid growth of shear stress, softening of shear stress after peak, and residual stability; (2) the peak strength of both interfaces increases initially and then decreases with an increase in water content, while residual strength is relatively less affected by water content; (3) peak strength and residual strength are linearly positively correlated with normal stress, and the strength of ice bonding is less affected by normal stress; (4) the mechanical properties of the cast-in-place concrete-frozen soil interface are significantly better than those of the precast concrete-frozen soil interface. However, when the water content is high, the former's mechanical performance deteriorates much more than the latter, leading to severe strength loss. Therefore, in practical engineering, cast-in-place concrete construction is preferred in cases of higher negative temperatures and lower water content, while precast concrete construction is considered in cases of lower negative temperatures and higher water content. This study provides reference for the construction of frozen soil-structure interface in cold regions and basic data support for improving the stability and service performance of cold region engineering.

토양칼럼을 이용한 초기우수 중 염양염류의 수변녹지 토양에서의 제거도 평가 (Soil Column Experiment to Evaluate Removal of Nutrients in Stormwater Runoff by Soil of Riparian Protection Zone)

  • 윤석표;최지용
    • 한국물환경학회지
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    • 제20권3호
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    • pp.231-235
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    • 2004
  • To investigate removal effects of nutrients in stormwater runoff by soil of riparian protection zone, soil column experiment was conducted for 20 months. Artificial stormwater runoff containing phosphate and nitrate was applied on the surface of soil column twice a week, and phosphate and nitrate concentrations were measured from the leached water. Soil of riparian protection zone reduced the released amount of infiltrated water to the surrounding water. After infiltration of 1m depth of soil column, average removal rates of phosphate and nitrate were 97.7 % and 74.7 %, respectively. As main mechanisms of phosphate are adsorption to soil particle and utilization by plants, periodical replacement of soil and harvesting of plant at the end of growing season are required. For the removal of nutrients in stormwater runoff by the soil layer, soil of riparian protection zone has higher hydraulic conductivity to infiltrate stormwater. Sandy soil having hydraulic conductivity of about $1{\times}10^{-2}cm/s$ range might be appropriate for this purpose.