• Journal of Korean Society of Forest Science
• /
• v.86 no.1
• /
• pp.98-104
• /
• 1997

Soil pollution intensity at Mt. Namsan in Seoul city which was expected to show significant soil contamination due to long-term air pollution was evaluated by comparing soil chemical properties at Mt. Kyebangsan in Hongcheon area as a control, and the bacteria participating in nitrogen or sulfur mineralization were assayed simultaneously in order to evaluate the validity of N and/or S mineralization bacteria as an index of soil contamination. The soil of Mt. Namsan showed 10 times higher concentration of hydrogen ion compared to that of Mt. Kyebangsan, which indicated that the soil had relatively been acidified seriously. Especially, large amount of canons were thought to be leached out from the soil, while the amount of extractable Al was getting larger and larger, which result in serious problems in soil ecosystem of the mountain. I could infer from soil chemical properties of the four study sites that the major reason of soil acidification was SOx deposition. However, the sulfur-reducing bacteria were not significantly different between the two regions, which indicated that the microbial dynamics of the soil ecosystem was not controlled by simple factor, but by multiple factors. By the way, the dynamics of bacteria participating in denitrification process was different between the two regions, which was more active at Mt. Kyebangsan than at Mt. Namsan. Thus, the microbial assay for nitrogen mineralization is desirable to be examined as a tool for evaluating soil health or microbial activity in soil ecosystem.

• Proceedings of the KIEE Conference
• /
• 2005.07a
• /
• pp.703-705
• /
• 2005

접지설계에 있어서 토양의 전기적 특성은 접지극의 형상과 더불어 가장 중요한 설계요소 중 하나이며 이러한 토양의 전기적 특성은 접지극이 매설될 지역의 고유한 저항률, 즉 고유저항률(specific earth resistivity)로 대표되어 왔다. 이처럼 고유저항률에 근거한 수작업 접지설계는 복잡한 구조와 특성을 갖는 실제 토양을 균일한 매질로 등가화하는 절차를 필요로 한다. 본 논문에서는 미얀마 500 kV 송전철탑 수작업 접지설계를 위하여 수평다층토양을 균일매질로 등가화하는 절차를 제시하였다.

• Proceedings of the Korea Water Resources Association Conference
• /
• 2004.05b
• /
• pp.1032-1036
• /
• 2004

수자원계획수립시 가장 큰 문제점 중의 하나는 관심대상유역의 관측자료가 없는 경우이다. 이와 같은 미계측유역의 경우 통상 단순히 인근관측소 자료를 면적비로 전이시켜 사용하거나, 인근 계측유역에서 유출모형의 매개변수를 추정하여 매개변수를 전이시키는 방법을 사용하고 있다. 본 연구에서는 계측유역에서 추정한 장기유출모형의 매개변수를 미계측유역으로 전이시킬 때 유역별 토양수분보유능을 이용하여 보다 객관적으로 매개변수를 전이하는 방법을 제시하였다. 방법으로는 정교한 토양수분모의가 가능한 PRMS 모형을 이용하여 자료의 정도가 높은 5개 댐지점에서 매개변수를 검${\cdot}$보정한 다음, 소양강댐과 충주댐유역을 미계측유역으로 가정하여 계측유역의 토양수분보유능과 가장 유사한 유역에 매개변수를 전이하여 결과를 분석하였다.

• Journal of Applied Biological Chemistry
• /
• v.63 no.3
• /
• pp.275-282
• /
• 2020

As pesticide safety was extended to agricultural environments and Positive List System was carried out, Pesticide safety management in soils has become even more important. To improve pesticide safety in soils needs the degradation technology of the residues in soils and reduce plant uptake of pesticides. In this study, biochars and quicklime as the degradation methods of pesticides (azoxystrboin, procymidone and tricyclazole) were used to identify the reduction effects. The experimental methods were putting biochars and quicklimes (0, 0.5, 1.0, 2.0% per 15 cm soil weight) in soils and analyzing the pesticide residues at 0, 10, 20, 35, 50 day. To identify the reduction effects of uptake from soil to korean cabbages (roots, leave, stems) by biochar treatment, the residues in samples were analyzed. As a results, azoxystrobin (36-96%), procymidone (40-117%) and tricyclazole (26-83%) were reduced in soils when treated with 2.0% quicklime (p<0.05). There were no reduction effect in soils when treated with 1.0% or less biochar. However, the amounts of residues translocated to roots (0.11-1.62 mg/kg), leave (0.05-0.29 mg/kg), stems (0.06-0.1 mg/kg) were reduced treated with 2.0% biochar treatments. The biochar and quicklime can be applicable to agricultural field to improve pesticide safety in soils.

• Journal of the Korean Geographical Society
• /
• v.50 no.2
• /
• pp.165-183
• /
• 2015

It is well known that, since the 15th century, the amount of soil loss in our country due to change in land use by human has increased more rapidly than ever before. However we cannot answer the question 'How long can the soil persist under the current rates of soil loss?', because it was difficult to quantify the soil production rate. With the advancement of accelerated mass spectrometry, the attempt to quantify rate of soil production and derive soil production function succeeded, and recently it was also applied into the Daegwanryeong Plateau. Here we introduce the principles for quantifying soil production and deriving soil production function using terrestrial cosmogenic nuclides, and then compare the soil production rates from the plateau with soil loss data after the late 20th century, and finally estimate how long the soil can persist. Averaged soil production rate since the Holocene derived from the plateau is revealed as ${\sim}0.05[mm\;yr^{-1}]$, and, however, the recent soil loss rate of intensively used farmlands at the same region is up to sixty times greater than the soil production rate. Thus, if current land use system is maintained, top soils on the cultivated lands over hillslopes especially in upland areas are expected to disappear within several decades at the earliest.

• Korean Journal of Environmental Agriculture
• /
• v.38 no.3
• /
• pp.119-123
• /
• 2019

BACKGROUND: Estimation of soil nitrogen supply is essential to manage nitrogen fertilization in arable land. In Korea, nitrogen fertilization is recommended based on the soil organic matter content because it is difficult to assess nitrogen (N) mineralization of upland soils directly. In this study, the relationship between soil organic matter (SOM) content and N mineralization was investigated to explore the limitation of using SOM in predicting soil N mineralization. METHODS AND RESULTS: Soil samples from the 0 to 10 cm depth were collected from 18 individual pepper cultivated fields in Tae-an and Chung-yang provinces before fertilization. N mineralization in the soils was quantified using incubation for 70 days at $30^{\circ}C$. The mineralizable soil N (MSN) was positively correlated with SOM, and the relation equation between MSN and SOM was '$MSN(kg\;10a^{-1})=0.2933{\ast}SOM(g\;kg^{-1})+0.0897$ ($r^2=0.6224$, p<0.001)'. However, the differences of N mineralization among the soils with the similar concentrations of soil organic matter were about 3 to 4.6 times, suggesting that the other soil factors such as total N concentration or EC should affect N mineralization. CONCLUSION: We concluded that SOM alone could not reflect the capacity of soil to supply N that is used for recommendation of N fertilization rate. Therefore, other soil properties should be considered to improve N fertilization management in arable land for sustainable agriculture.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
• /
• 1996.04a
• /
• pp.70-73
• /
• 1996

• Korean Journal of Soil Science and Fertilizer
• /
• v.25 no.3
• /
• pp.293-296
• /
• 1992

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
• /
• 1996.11a
• /
• pp.144-147
• /
• 1996

• Journal of the Korean Geographical Society
• /
• v.18
• /
• pp.1-12
• /
• 1978

이 글에서는 다음의 내용을 다루었다. 1. 토양교질물의 화학분석 결과 및 고찰 2. 토양생성화 작용과 규반 비.규철반비와의 관계