• 한국토양비료학회지
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• 제43권1호
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• pp.1-7
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• 2010

본 연구는 논토양 쟁기바닥층을 대상으로 특성을 파악하고 토양입자분포를 프랙탈차원화하여 물이동을 추정하고자 수행하였다. 모내기전 비담수기에 보통논과 사질논 12지점을 각각 선정하였다. 선정지점에서 깊이별 관입경도를 측정하여 쟁기바닥층 출현깊이와 두께를 도출하였다. 표토와 쟁기바닥층에서 토양입자분포, 유기물함량, 산중식 경도를, 쟁기바닥층에서 2인치 코아시료를 채취한 후 변수위법으로 포화수리전도도를 측정하였다. 토양입자분포의 프랙탈 차원화는 측정한 입자분포자료, 0-0.002, 0.002-0.053, 0.053-0.1, 0.1-0.25, 0.25-0.5, 0.5-1.0, 1.0-2.0 mm의 함량을 활용하여 Tyler와 Wheatcraft (1992)의 방법을 따랐다. 조사한 연구지점의 쟁기바닥층 출현깊이는 5-30 cm, 두께는 5-17 cm로 분포하였으며 보통논이 사질논보다 평균적으로 출현깊이가 깊고 두께는 얇은 것으로 나타났다. 또한 보통논은 점토함량이 18%이상으로 상대적으로 세립질 토성을, 사질논은 18%이하로 조립질 토성을 나타내었다. 토양입자분포의 프랙탈차원 ($D_m$)은 세립질 토성일수록 높은 값을 나타내었으며 조립질토양에서 더 높은 프랙탈성을 나타내었다. 포화수리전도도는 0.5-1420 mm $day^{-1}$로 분포하였으며 사력질 사질논에서 가장 높은 값을 나타내었다. 포화수리전도도는 점토함량과 $D_m$이 증가함에 따라 감소하는 경향이 나타났으며 멱함수의 형태를 나타내었다. 점토함량보다 $D_m$을 독립변수로 사용했을시, 적합된 멱함수의 결정계수가 높았으며 특히 사질논이 보통논보다 결정계수가 높게 나타났다. 따라서 본 연구는 토양입자분포를 프랙탈 차원화를 통해 단일 값으로 표현하여 포화수리전도도 등의 물이동 특성 추정에 활용할 수 있다고 보여준다 할 수 있다. 특히 조립질 토성을 가진 논토양의 물이동 추정에 유용할 것으로 판단할 수 있었다.

• 한국토양비료학회지
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• 제49권4호
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• pp.300-309
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• 2016

The monolithic weighing lysimeter is a useful facility that could directly measure water movement via layers, drainage, and evapotranspiration (ET) with precise sensors. We evaluated water movement through layers and water balance using the lysimeter with undisturbed paddy sandy loam soil, Gangseo soil series (mesic family of Anthraquic Eutrudepts classified by Soil Taxonomy) during winter season from Dec. 2014 to Feb. 2015. Daily ET indicated up to 1.5 mm in December and January and 2 mm in February. The abrupt increase of soil water tension at the depth of 0.1 m, when soil temperature at the same depth was below $2^{\circ}C$, was observed due to temporary frost heaving. The surface evaporation was less than reference ET below -15 kPa of soil water potential at the depth of 0.1 m. The maximum drainage rate was similar to the saturated hydraulic conductivity of a plow pan layer. Both upward and downward water movement, related to ET and drainage, were retarded by a plow pan layer. This study demonstrated that the lysimeter study could well quantify water balance components even under frost heaving during winter season and that a plow pan with low permeability could act as a boundary that affects drainage and evapotranspiration.

• 한국토양비료학회지
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• 제49권6호
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• pp.655-661
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• 2016

Relationships between saturated conductivity (Ks) and separate contents were evaluated from 44 soil series of arable lands: 18 for paddy fields and 26 for upland crop fields. Saturated hydraulic conductivities of A, B, and C horizons were determined with tension infiltrometer and Guelph permeameter in situ. Sand, silt, clay, and organic matter content of each horizon were analyzed. Based on correlation analysis, sand separate had a positive relationship with Ks for both paddy (r=0.27, p=0.017) and upland fields (r=0.24. p=0.030). Clay content had a negative relationship with Ks for paddy soils (r=-0.32, p=0.005) while significant correlation between them was not found for upland crop fields (r=-0.20, p=0.07). Organic matter content showed a positive relationship with Ks only for upland crop fields (r=0.33, p=0.002). Due to low correlation coefficients between separate contents and Ks, performance of pedotransfer functions was not enough to estimate Ks. It implies that hydraulic properties of arable lands were affected by other factors rather than particle characteristics. Platy structure and plow pan were suggested to limit Ks of paddy fields. Soil compaction and diversity of parent materials were proposed to influence Ks of upland crop fields. It suggests that genetic processes and artificial managements should be included in pedotransfer functions to estimate hydraulic properties appropriately.

• 한국토양비료학회지
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• 제48권4호
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• pp.246-254
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• 2015

This study explored the effect of rainfall pattern and soil characteristics on water management in rice paddy fields, using a soil water balance model, BUDGET. In two sites with different soil textural group, coarse loamy soil (Gangseo series) and fine soil (Hwadong series), respectively, we have monitored daily decrease of water depth, percolation rate, and groundwater table. The observed evapotranspiration (ET) was obtained from differences between water depth decrease and percolation rate. The root mean square difference values between observed and BUDGET-estimated ET ranged between 10% and 20% of the average observed ET. This is comparable to the measurement uncertainty, suggesting that the BUDGET model can provide reliable ET estimation for rice fields. In BUDGET model of this study, irrigation requirement was determined as minimum water need for maintaining water-saturated soil surface, assuming 100 mm of bund height and no lateral loss of water. The model results showed different water balance and irrigation requirement with the different soil profile and indicated that minimum percolation rate by plow pan could determine the irrigation requirement of rice paddy field. For the condition of different rainfall distribution, the results presented different irrigation period and amounts, representing the importance of securing water for irrigation against different rainfall pattern.

• 한국토양비료학회지
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• 제40권4호
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• pp.330-348
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• 2007

한국의 간척지에서 토양 문제와 농업 용수 관리에 대해 농촌진흥청과 농업기반공사 등에서 이루어진 연구를 통해 얻어진 결과를 토대로 하여 개관하였다. 한국토양분류와 조사에 의하면, 5개 토양목의 45개 토양통이 서남해안의 하해혼성 또는 해성 퇴적지에 분포하고 있었다. 염포, 문포, 하사, 광활, 포승통이 해안의 간석지에 연접한 하해혼성 퇴적지에 가장 많이 분포하고 있는 토양통들이었다. 염포 등 앞의 4개 토양통은 엔티솔이며, 포승통은 인셉티솔이었다. 포승통과 연접한 부용통 등은 알피솔이었다. 몰리솔인 명지통, 히스토솔인 용호통 등의 분포 면적은 적었다. 염류도 제어와 관리 문제는 높은 지하수위와 미사가 많은 간척지 토양에서 제염 과정에서 생성된 경운 반층에 의한 낮은 투수 속도와 밀접한 관련이 있다. 포장에서 염류의 평가에 있어서 GPS와 결합된 전자장 유도 EM38이 염류도와 포장 변이를 이해하는 데 유용하였다. 심경, 심토 파쇄, 암거에 의한 배수 개선 등은 경운 반층이 형성된 논에서 효과적이었다. 변량 시비와 같은 신기술은 비료를 절감하고 수질에 대한 농업 영향을 감축시킬 가능성이 있었다. 간척지에서 농업용수의 수질은 내륙 수자원의 수질보다 열악하였다. 작물 생육에 알맞은 수질과 함께 목표 수질 달성에 맞추어 갈 수 있는 작물 관리가 필요하였다.

• 한국토양비료학회지
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• 제48권6호
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• pp.641-647
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• 2015

Monitoring of soil fertility by long-term application of fertilizers is necessary to improve the fertility of soil and the productivity of crop. The objective of this study was conducted to investigate the changes of exchangeable Mg by continuous application of fertilizers from 1969 to 2014. The treatments were no fertilization (No fert.) and fertilization (NPK, NPK+C, NPK+S, and NPK+CS). The concentration of exchangeable Mg in No fert., NPK+C, and NPK+S treatments tended to increase from 1965 to 1975, but decrease gradually from 1976 to 1987, and increase again after 1988. Based on these, the changes of exchangeable Mg were divided into period I ('69 ~'75), period II ('76~'87), and period III ('88~'14). Especially, exchangeable Mg decreased in the period II. This was presumed that a significant amount of Mg from topsoil were leached into subsoil by break of plow pan and some of subsoil was incorporated into topsoil according to change of plowing depth by replacement of tillage machinery. It could be possible that exchangeable Mg in NPK, NPK+S, and NPK+CS was accumulated in the depth of 15~20 cm. For the period III, exchangeable Mg in No fert., NPK, NPK+C, NPK+S, and NPK+CS treatments increased at rates of 0.013, 0.018, 0.015, 0.023, and $0.024cmolckg^{-1}{\cdot}yr^{-1}$ respectively. Exchangeable Mg level in NPK+S was lower than the other treatments in the period I and period II, but higher than in the period III. This result was attributed to replacement of silicate fertilizer type from wollastonite (Mg 0.3%) to silicate fertilizer (Mg 3%). Also, exchangeable Mg level of No fert. treatment increased, which showed that Mg concentration of irrigated water had the greatest impact on Mg accumulation of soil. Recently, Mg level of irrigated water tended to increase, indicating that Mg concentration of water will affect greatly the concentration of exchangeable Mg of soil in the future. Like these, the changes of exchangeable Mg were greatly influenced by agricultural environment such as plowing depth, plow pan, content of fertilizer, and quality of irrigated water. Considering these agricultural environment, the proper management of soil is needed for the improvement of soil fertility and crop productivity.

• 한국토양비료학회지
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• 제50권5호
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• pp.336-344
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• 2017

The soil water characteristics curve (SWCC) represents the relation between soil water potential and soil water content. The shape and range of SWCC according to the relation could vary depending on soil characteristics. The objective of the study was to estimate SWCC depending on soil types and layers and to analyze the trend among them. To accomplish this goal, the unsaturated three soils were considered: silty clay loam, loam, and sandy loam soils. Weighable lysimeters were used for exactly measuring soil water content and soil water potential. Two fitting models, van Genuchten and Campbell, were applied. Two models entirely fitted well the measured SWCC, indicating low RMSE and high $R^2$ values. However, the large difference between the measured and the estimated was found at the 30 cm layer of the silty clay loam soil, and the gap was wider as soil water potential increased. In addition, the non-linear decrease of soil water content according to the increase of soil water potential tended to be more distinct in the sandy loam soil and at the 10 cm layer than in the silty clay loam soil and at the lower layers. These might be seen due to the various factors such as not only pore size distribution, but also cracks by high clay content and plow pan layers by compaction. This study clearly showed difficulty in the estimation of SWCC by such kind of factors.