• 한국환경농학회지
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• 제37권3호
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• pp.166-171
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• 2018

중량식 라이시미터를 활용하여 배추 재배 중 식양토와 사양토의 질소 용탈과 질소 수지를 평가하였다. 생육 초기인 9월 초 강우로 인해 식양토와 사양토 모두 토심 150 cm 이하로 배수가 있었다. 식양토는 점토의 수축 및 작물 뿌리 등에 의해 형성된 대공극을 통해 일시적으로 배수량이 증가하였으나, 사양토는 식양토와 달리 강우량에 따라 일정하게 배수량이 증가하고, 감소하였다. 토성별로 질소 용탈량을 분석한 결과, 식양토에서는 비료의 용탈이 거의 없는 반면, 사양토에서는 식양토에 비해 5배 많은 질소 용탈이 있었다. 질소수지에서 작물 흡수량에 비해 질소 용탈량이 차지하는 비율은 적었으나 식양토에 비해 사양토에서의 용탈량이 많아 질소 수지 산정에 토성에 따른 용탈특성을 고려할 필요가 있다.

• 한국토양비료학회지
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• 제49권5호
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• pp.564-571
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• 2016

As the amount of rice straw collected increases, green manure crops are used to provide the needed organic matter. However, as green manure crops generate methane in the process of decomposition, we tested with different tillage depths in order to reduce the emission. The atmosphere temperature of the chamber was $25{\sim}40^{\circ}C$ during the examination of methane and soil temperature was $2{\sim}10^{\circ}C$ lower than air temperature. The redox potential (Eh) of the soil drastically fell right before irrigated transplanting and showed -300~-400 mV during the cultivating period of rice (7~106 days after transplant). When hairy vetch was incorporated to soil and the field was not irrigated, the generation of methane did not occur from 12 to 4 days before transplanting rice and started after irrigation. Regarding the pattern of methane generation during the cultivation of rice, methane was generated 7 days after transplanting, reached the pinnacle at by 63~74 days after transplanting, rapidly decreased after 86~94 days past transplanting and stopped after 106 days past transplanting. When tested by different soil types, methane emission gradually increased in loam and clay loam during early transplant, whereas it sharply increased in sandy loam. The total amount of methane emitted was highest in sandy loam, followed by loam and clay loam. In all three soil types, methane emission significantly reduced when tillage depth was 20 cm compared to 10 cm. The rice growths and yield were not affected by tillage depth. Therefore, reduction of methane emission could be achieved when application hairy vetch to the soil with tillage depth of 20 cm in paddy soil.

• 한국환경농학회지
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• 제19권1호
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• pp.67-71
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• 2000

재배년수와 토성이 도라지 생육 및 수량에 미치는 영향을 연구한 결과는 다음과 같다. 재배년수가 2년에서 8년까지 양질사토에서 시험한 결과 재배년수와 1근중은 $Y=17.246X+0.95(R^2=0.948^{{\ast}{\ast}{\ast}})$, 발병율은 $Y=12.01X-5.74(R^2=0.946^{{\ast}{\ast}{\ast}})$로서 고도의 유의성이 있었다. 재배년수가 길수록 뿌리의 T-N, $P_2O_5$, MgO 함량은 감소되었고 장해근은 정상근에 비해 T-N, $P_2O_5$, $K_2O$ 함량이 높았다. 도라지 2년생을 양질사토, 사양토, 미사질양토와 식양토에서 시험한 결과 시험후 pH는 미사질양토가 6.4였으며 다른 토성에서는 $5.7{\sim}5.8$의 수치를 나타내었고 $P_2O_5$ 및 Fe 함량은 미사질양토에서 높았다. 도라지 생육상황은 미사질양토에서 지상중 10.38g, 근경 1.34cm, 근장 16.8cm, 초장 57.9cm로 양호하여 1근중이 5.46g으로 가장 높았다.

• Journal of Ecology and Environment
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• 제37권2호
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• pp.61-67
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• 2014

Mankyua chejuense is a native endangered plant distributed only in Gotzawal, a forested wetland, in Jeju Province, Korea. In order to determine the optimal environmental conditions for the growth and development of M. chejuense, we investigated the above- and below-ground growth responses and survival rate to various soil texture (sand and clay), water regimes (flooding and non-flooding), and $CO_2+T$ (ambient and elevated) conditions. All of the treatments had significant effects on aboveground growth parameters, while only the water regime and $CO_2+T$ treatments influenced belowground growth. The survival rate of M. chejuense was about twice higher under the sand, non-flooding and elevated $CO_2+T$ conditions than clay, flooding and ambient $CO_2+T$ conditions. These results indicate that M. chejuense grows in well-drained sandy soil conditions and elevated $CO_2$ concentration and temperature situations. Thus, there is a need to maintain M. chejuense under constant non-flooding soil conditions by implementing appropriate soil drainage strategies.

• 한국토양비료학회지
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• 제16권2호
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• pp.126-130
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• 1983

토양의 물리적(物理的) 특성(特性)이 작물(作物)의 뿌리 발달에 미치는 영향(影響)을 구명(究明)하기 위하여 배수등급(排水等級), 토성조건(土性條件)이 상이(相異)한 대맥포장에서 토양물리성과 층위별(層位別) 뿌리 분포(分布)를 조사(調査)한 결과(結果)는 다음과 같다. 1. 배수(排水)가 양호(良好)할수록 총뿌리량은 증가(增加)되고 깊게 분포(分布)하였으며 동일(同一)한 배수등급(排水等級)에서는 토양이 세립질(細粒質)일수록 총뿌리량이 많은 경향(傾向)이었다. 2. 토양의 경도(硬度)는 가비중과 밀접(密接)한 관계가 있었으며 토성(土性)이 세립질(細粒質)일수록 유의성(有意性)이 높았다. < 식토(埴土) ($r=0.837^{**}$), 식양토($r=0.678^*$), 사양토($r=0.654^*$) > 3. 심토(深土)의 가비중과 뿌리량과는 고도(高度)의 유의성(有意性)있는 부(負)의 상관($r=-0,846^{**}$)이 있었으며 가비중이 $1.4g/cm^3$이상(以上) 되면 대맥 뿌리 발달은 현저(顯著)히 떨어졌다. 4. 심토(深土)의 가비중은 배수(排水)가 불량(不良)하고 토성(土性)이 조립질(組粒質) 일수록 감소(減少)되었으며 특(特)히 배수(排水)가 약간불량(若干不良)한 경우(境遇)와 약간(若干) 양호(良好)한 식토(埴土)에서는 기상이 20% 미만(未滿)으로 작물(作物) 생육(生育)이 불량(不良)하였다. 5. 대맥의 뿌리 신장(伸長)에는 표토(表土)는 경도(硬度), 토심(土深) 10~30cm는 가비중과 기상, 30~50cm는 기상의 영향(影響)이 컸다.

• 한국토양비료학회지
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• 제49권6호
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• pp.705-711
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• 2016

Crimson clover, a legume crop, is a landscape crop and green manure crop that can be sowing in spring and autumn. Its red flower blooms in May, and serves various roles such as landscape composition, weeds suppressing, prevention of soil loss and nutrient on sloping land and supplying nitrogen and organic matter in soil. Thus, in order to utilize this crop in agriculture land, we evaluated the growth characteristics of crimson clover cultivated in four different soil textures; sand, sandy loam, loam, and clay loam. The nitrogen content of crimson clover was $15.8g\;kg^{-1}$ and C/N ratio was 20.3. Its plant height was 42.5 cm in sandy loam and 49.5 cm in loamy, respectively, approximately 20 cm longer than the sand and clay loam. The crimson clover in sandy loam and loam bloomed about seven days earlier than those in sand and clay loam. Regarding number of flower per hill and flower length, there were no difference among the soil textures. Dry weight of crimson clover for sandy loam and loam was $2.5Mg\;ha^{-1}$ and $2.3Mg\;ha^{-1}$, respectively, $0.8{\sim}1.1Mg\;ha^{-1}$ higher than that of sand and sandy loam. Plant height and dry weight of crimson clover increased with delaying harvest time. Nitrogen contribution in loam and clay loam was $51.3kg\;ha^{-1}$ and $53.5kg\;ha^{-1}$, respectively. Therefore, in terms of flowering properties and dry weight, the proper soil texture for the growth and development of crimson clover was sandy loam and loam.

• 농업과학연구
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• 제49권2호
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• pp.379-387
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• 2022

A large amount of the mineral nitrogen is necessary for crop growth. With the use of nitrogen fertilizers, agricultural yield has increased during the last few decades. However, at the same time, nitrate from the cultivated land can be a source of environmental pollution, especially in water systems. For nitrogen management, it is necessary to analyze the pattern of nitrogen movement in soil. In this study, nitrogen leaching in upland soils was evaluated using undisturbed lysimeters with different soil textures during sesame cultivation. The soil texture of the lysimeters was clay loam (Songjung series) and sandy loam (Sangju series) soils. Sesame was cultivated from May 25 to August 24 in 2020. The standard amount of NPK fertilizer (N-P₂O₅-K₂O = 2.9-3.1-3.2 kg·10 a^-1) was applied before sowing. The amount of nitrogen leaching was calculated by multiplying the nitrogen (NO₃-N + NH₄-N) concentration and the amount of water drained below 1.5 m soil depth. The water was drained through percolation into macropores in the clay loam lysimeter. In contrast, in the sandy loam lysimeter, water drained more slowly than in the clay loam lysimeter. There was a slight difference in the total amount of leachate during the cultivation period, but the amount of nitrogen leaching was high in sandy loam soil. During the sesame cultivation period, the amount of nitrogen leaching from clay soil was 5.64 kg·10 a^-1, and 10.70 kg·10 a^-1 for sandy soil. We found that there was a difference in leaching depending on the soil physical characteristics. Therefore, it is necessary to consider the characteristics of soil to evaluate the leaching of nitrogen.

• Current Research on Agriculture and Life Sciences
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• 제21권
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• pp.39-47
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• 2003

아까시나무 조림이 토양에 미치는 영향을 파악하기 위하여 아까시나무 조림지와 인접하고 있는 다른 임분의 토양 이화학적 성질을 비교, 분석하여 토양특성의 변화에 대해 조사하였다. 아까시나무 조림지와 인접 임분의 토성은 대부분 사양토와 양질 사토로 나타났다. 토양 pH, 유효인산의 함량, 탄소와 전질소의 함량이 아까시나무 조림지와 인접 임분사이에 차이가 있음을 확인할수 있었다. 아까시나무 조림지에서 토양 pH와 탄소의 함량은 참나무류림보다는 낮지만, 소나무류림보다는 높았으며, 유효인산과 질소의 함량은 아까시나무 조림지가 인접 임분보다 높게 나타났다. 각 임분들 사이에서는 토양 pH가 높은 통계적인 유의성을 보였으며, 탄소와 전질소함량에서도 통계적인 유의성이 있었다. 또한 토양 pH, 탄질률, CEC, 전질소함량 순으로 높은 상관관계를 보였다. 아까시나무가 인접하고 있는 참나무류림과 소나무류림에 침입하는 정도를 다르게 할 수 있다고 추론할 수 있었다.

• 유기물자원화
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• 제10권2호
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• pp.132-139
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• 2002

본 연구는 디젤의 오염기간 및 토성이 콤포스팅 처리효율에 미치는 영향을 살펴보고자 실시하였다. 오염경과기간은 15일과 60일로 하였으며 대조실험으로 오염직후의 토양실험도 실시하였다. 연구에 사용된 토양은 실트질양토와 사토이었으며 대상오염물질은 디젤오일이었다. 초기오염농도는 건조질량기준으로 약 10,000mgTPH/kg으로 하였으며, 수분은 각 토성의 수분보유능력의 70%로 조절하였다. 유기물질 보충 및 미생물식종의 목적으로 하수슬러지를 첨가하였으며 토양대 슬러지 혼합비율은 습윤질량비로 1:0.3이었다. 휘발된 TPH양은 초기농도의 0.9-1.8%정도로써 디젤오염토양의 콤포스팅 적용시 디젤은 주로 생물학적인 요인에 의하여 제거되었다. 휘발에 의하여 손실되는 n-alkanes들은 대부분 C10~C17의 성분들이었으며, 특히 C10~C14까지의 성분들이 C15 이상의 성분들보다 휘발이 많이 되었다. 사토의 TPH에 대한 1차반응 분해속도상수 k값은 0.081-0.094/day로 실트질양토의 0.056-0.061/day보다 약 1.5배 정도 높았다. 오염경과기간의 영향을 살펴보면, 60일까지의 오염경과기간으로는 TPH 분해효율의 뚜렷한 차이를 발견할 수 없었다. 이산화탄소회수율은 0.61-0.89이었으며, TPH분해량과 이산화탄소발생량과의 상관계수는 0.90-0.96의 범위에 있었다.

• The Korean Journal of Ecology
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• 제21권5_3호
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• pp.649-663
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• 1998

The clarify the ecological properties, and to predict change of understory vegetation of mt. Nam Park, population dynamics and interspecific competition of D. smilacinum and D. viridescens, which grow in understory of deciduous broad-leaved forest and pseudo-annuals, were studied from May 20 to May 30 1998. The depth of litter layer, soil moisture content, soil organic matter and soil texture were surveyed in 18 populations (15 D. smilacinum populations and 3 D. viridescens populations). Mean litter layer of d. smilacimum population was thinner than that of D. viridescens populations). Mean litter layer of D. smilacnum population was thinner than that of D. viridescens population. The contents of soil moisture and organic matter of D. smilacinum population were lower than that of D. viridescens population. The D. smilacinum growed in broad range of soil texture but D. viridescens in loamy soil. Because D. smilacinum could tolerate more broad range of soil moisture and soil texture than D. viridescens, the former covered the herb layer in earlier stage and the latter introduced in later stage when rhizome could grow easily. The numbers of individual in two marginal parts were smaller than that in center in same D. smilacinum patch. And the total numbers of individuals grown in (10 ${\times}$ 10)cm were from 0 to 12. The rhizome (subterranean runner) weight, rhizome length, root weight, shoot weight, lea weight and leaf number per subquadrat (cell) increased along the number of individual, that is, increased from marginal part to center. But rhizome weight and rhizome length per individual were vice versa. Therefore, the individuals in marginal part reproduced longer and stronger asexual propagules than that in center. The distribution pattern of D. smilacinum was contageous and that of D. viridescens was random or regular. Therefore, population growth of former was independent on density and that of latter was dependent on density. The distributions of size-class showed normal curves in two population, but the curves based on data of total dry weight showed positive skewness and those of leaf number showed negative skewness The correlation coefficient (CC) values between the properties of each organ were high in two population and significant at 0.1% level. The CC values of D. viridescens were higher of the two. Therefore, the former allocated the energy to each organ stable. The rhizome depth of d. viridescens was 2 times deeper than that of D. smilacinum. And rhizome length and weight of D. viridescens were longer (2 times) or heavier (4 times) than those of D. smilacinum. The patch size of D. viridescens increased 60 cm per year and that of D. smilacinum 30 cm. On this results, the intrinsic increase velocity of d. viridescens patch was 2 times faster than that of d. smilacinum, therefore, on the competition, the former had an advantage over D. smilacinum. The reason why d. viridescens defeated D. smilacinum resulted from that the leaf area of former was 4 times broader than that of latter. in Mt. Nam Park, it was thought that two disporum Population would change with the 3 thpes of environmental change as followings. First, no human impact and increase of soil moisture content resulted in increase of D. viridescens population. Second, mild human impact and similar condition of soil moisture content resulted in slow increase or no changes of D. smilacinum and d. viridescens population. Third, severe human impact and dry condition resulted in decrease or vanishment of two disporum populations.