• Proceedings of the Korean Society for Bio-Environment Control Conference
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• 2001.04b
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• pp.67-68
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• 2001

돈분발효퇴와 포도주 부산물의 질소 무기화 및 질산화 과정을 구명하기 위해 시설 내 고추생육시기에 토층별 암모늄태 및 질산태 질소함량을 조사하였다. 질소무기화 및 질산화는 심토층보다 표토층에서 높게 나타났다. 생육전반에 걸쳐 총 질소 무기화 및 질산화율은 처리간에 다양하였지만, 전반적으로 총 질소 무기화는 정식후 90일 까지 증가하였지만 그 이후로는 감소하였다. 표토층에 있어 최고 질소 무기화 및 질산화는 정식후 90일에 T4(포도주부산물 400kg/10a＋돈분발효퇴비 1,000kg/10a)에서 관측되었다. 가장 높은 질소 무기화는 정식후 30일에 대조구에서 272.5mg/kg과 정식 후 90일에 T4(포도주부산물 400kg/10a＋돈분발효퇴비 1,000kg/10a)에서 843.4mg/kg으로 나타났다. 또한 질산화는 T4(포도주부산물 400kg/10a＋돈분발효퇴비 1,000kg/10a)에서 정식 후 90일에 872.2mg/kg으로 가장 높게 나타났다. 15-30cm 토층의 질산화 현상은 질소 무기화와는 다르게 나타났는데 질소 무기화는 대체로 90일에 증가한 반면 질산화는 90일에 감소하는 경향을 나타내었다. 마지막 조사시기인 정식 후 180일에는 급격히 감소하는 현상을 보였는데 고추 생육에 따라 양분 흡수로 암모늄태질소 및 질산태질소가 감소되었다. 0-15cm 토층, 15-30cm 토층의 질소무기화 및 질산화에서 T4(포도주부산물 400kg/10a＋돈분발효퇴비 1,000kg/10a)의 15-30cm 토층 질산화가 낮게 나타났다.

• Proceedings of the Korea Water Resources Association Conference
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• 2021.06a
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• pp.70-70
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• 2021

강수의 변동성 중 특히 가뭄과 홍수의 급격한 연간 변화는 기후변화로 인하여 근래에 많이 발생하고 있다. 가뭄이 발생한 이후 홍수가 발생하거나 그와 반대의 현상이 발생하는 것을 날씨 편달(weather whiplash)라고 한다. 이러한 현상은 토양에 매설되어 수분을 저감하는 배수시설로 인하여 토양 수분 변동 및 무기질소 손실에 지배적은 영향을 준다. 이러한 질소 손실은 부영양화를 일으켜 생태계에 막대한 영향을 미치게 된다. 하지만, 토양 무기질소는 토양에서 체류시간이 길기 때문에 강우 변동성에 의해 발생하는 상호작용을 특정하고 분석하기에는 많은 어려움이 따른다. 이 문제를 해결하고자 이번 연구에서는 생태수문모형과 생물지질모형을 결함한 3차원 모델인 Dhara를 이용하여 토양 배수시설에서 유출되는 무기 질소의 농도 및 나이를 분석하였다. 여기서 나이란 화합물이 발생 하여 다른 형태로 변화하는데 걸리는 시간을 의미한다. 집중적으로 관리되는 경작지에 Dhara 모형을 적용하여 본 연구를 수행하였다. 토양 수분과 질소의 나이를 분석한 결과 반응 화합물인 질소의 경우 토양 수분(비반응 화합물)과 비교하여 이전의 강우상태에 많은 영향을 받는 것으로 분석이 되었다. 가뭄이후 홍수가 발생할 때 배수시설에서 발생하는 질소의 유출이 그 반대 기상 환경인 홍수 이후 가뭄이 발생할 때 보다 더 많이 발생한 것으로 나타났다. 하지만 배수 흐름의 경우 질소의 거동과 반대하는 현상을 보였다. 이러한 결과는 질소유출 저감하여 강 및 바다에서 부영양화를 감소하기 위해 강수의 변동성과 연계하여 분석한다면 새로운 질소유출 저감 대책을 수립할 수 있는 가능성을 보여주었다.

• Journal of the Korea Organic Resources Recycling Association
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• v.15 no.1
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• pp.149-158
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• 2007

To investigate the characteristics of the nitrogen mineralization of oil cakes according to changes in temperature(10, 20, $30^{\circ}C$) moisture(40, 50, 60, 70% of field capacity in loam and 50, 60, 70, 80% of field capacity in sandy loam), mineral nitrogen was measured in soil after incubation for 30 days. In addition, the mineralization in sandy loam and loam which had different soil texture were compared. According to incubating the castor seed, soybean, and rice bran cakes with soil, the higher the temperature and moisture content were, the higher the content of mineral nitrogen was observed. The content of mineral nitrogen was higher in sandy loam than loam. The content of mineral nitrogen was decreased with soil depth increasing and was also higher in sandy loam than loam.

• Korean Journal of Soil Science and Fertilizer
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• v.38 no.5
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• pp.253-258
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• 2005

It is necessary to determine a nitrogen supplying capacity (NSC) of soil for sustainable agriculture. NSC has been decided by directly detecting N mineralization potential (NMP) and inorganic nitrogen or by indirectly approximating from organic matter and chemical properties of soil. NMP is best method for NSC but it takes long period. A study was conducted to find a short-term incubation method using pepsin through 1) determining NMP of 3 upland and 3 paddy soils, 2) establishing analytical condition of pepsin digestion by comparing to NMP, 3) validating with relations to N requirements for maximum yield of rice. NMPs of 6 soils were ranges from $63mg\;N\;kg^{-1}$ to $156mg\;N\;kg^{-1}$. The pepsin digestion method of soil nitrogen was established by determining amino nitrogen from digesting 5 g of soil for 30 minutes by 0.02% pepsin. This method was so highly correlated with a maximum rate of nitrogen fertilizer that it could be used for determining NSC in paddy soil.

• Korean Journal of Soil Science and Fertilizer
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• v.30 no.1
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• pp.23-28
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• 1997

A better understanding of nitrogen transformations in soils is essential to increase fertilizer nitrogen use efficiency. A laboratory incubation study was conducted to determine net mineralization and nitrification in selected Piedmont soils. Net mineralization and nitrification increased up to 60 days in the surface layers of Enon, Mecklenburg and Chewacla. After 60 days both processes declined up to 90 days incubation. In Wehadkee, mineralization and nitrification did not differ with incubation time. In all subsurface layers, mineralization and nitrification increased with time up to 90 days. Mineralization and nitrification differed among soils in surface and subsurface layers. These differences might be influenced by soil type related to amount of mineralization, soil aeration and nitrifying bacterial populations. A mineralization and nitrification was greater in surface layers than in subsurface layers.

• Korean Journal of Ecology and Environment
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• v.33 no.4 s.92
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• pp.350-357
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• 2000

This paper evaluated the influence of point source and flow events on inorganic nitrogen fractions at 17 sites of Taechung Reservoir during 1993${\sim}$1994. Total nitrogen (TN) averaged 1.53 mg/L during the study and ranged between 0.70 and 2.56 mg/L. Dissolved inorganic nitrogen(DIN) accounted for >90% of TN regardless of season and location, indicating a nitrogen-rich system showing eutrophic${\sim}$hypereutrophic conditions. Some 67${\sim}$94% of DIN was NO$_{3}$-N, whereas mean level of NH$_{4}$-N was less than 5% of DIN. During monsoon 1993, dilution of NO$_{3}$-N was evident in the headwaters as a result of mixing of lake water with rain water, while NH$_{4}$-N increased>100% compared to the premonsoon. Values of NH$_{4}$-N had a positive correlation with rainfall (r=0.85; p<0.001) and negative correlations with theoretical water residence time(r=-0.90; p<0.001) and conductivity(r=-0.78, p<0.001), respectively. These outcomes suggest that NH$_{4}$-N came from external input from the watershed during the monsoon. In both years, mean TN was greater in the mid-lake sites than any other sites. A great amount of TN in the mid-lake was most pronounced in monsoon 1994 because of an accumulated influence of the point sources during low inflow. Overall data suggest that concentrations of TN in this system did not show large differences along the longitudinal gradients and its distributions is likely determined by point-sources rather than inflow regime.

• Journal of Bio-Environment Control
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• v.10 no.4
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• pp.219-224
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• 2001

This experiment was conducted to evaluate net mineralization and nitrification in rain shelter soil incorporated with wine sludge. Net mineralization and nitrification rates varied among treatments during pepper growing periods. In general, net mineralization increased up to 90 days after transplanting before its decrease during the rest growing periods. Maximum net mineralization and nitrification in upper 0-15 cm layer soil were observed in T4 at 90 days after transplanting. The greatest amount of mineralization in upper layer soil was 272.5 mg.kg$^{-1}$ at 30 days in the control and 843.3 mg.kg$^{-1}$ at 90 days after transplanting in T4. Overall, both net mineralization and net nitrification were greater in the upper layer soil than in the lower 15-30 cm layer soil.

• Journal of Korean Society of Forest Science
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• v.87 no.1
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• pp.20-26
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• 1998

The objective of this study was to determine the rate of nitrogen mineralization and nitrification in a mature sawtooth oak(Quercus acutissima $C_{ARRUTH}$) stand in the Chungbu Forest Experiment Station, Kyonggi Province. Nitrogen mineralization and nitrification in the top 15cm of mineral soil were examined from November 1995 to November 1996 using an in situ buried bag method. Net nitrogen mineralization was 95.2mg/kg/yr and nitrification was 65.4mg/kg/yr. Nitrification consisted of 69% of annual nitrogen mineralization. Neither nitrogen mineralization nor nitrification was significantly correlated with the monthly soil temperature and soil moisture content.

• KOREAN JOURNAL OF CROP SCIENCE
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• v.20
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• pp.152-162
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• 1975

Five barley varieties were compared under six 1evels of nitrogen fertilization and two methods of cultural management, conventional and drill seeding. The increase in grain yield and nitrogen content of the leaves showed a significant linear regression from added increaments of nitrogen in Haganemugi and Olbori, particulary under drill seeding. The other varieties resulted in various degrees of lodging and no significant increases in yield. The spike number per square meter was the major component of yield, but when the spike number per square meter was sufficient, 1000 grain weight was equally as important as a component of yield.

• Journal of the Korea Organic Resources Recycling Association
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• v.6 no.2
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• pp.81-93
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• 1998

In order to estimate the an adequate application level for dry matter production of orchardgrass(Dactylis glomerata L.) were investigated in different application levels of food waste compost and mineral nitrogen in 3 cuttings per annum, and to evaluated the soil improving effect of food waste compost. Annual food waste compost and mineral nitrogen were applied at levels of 0, 10, 20, 40 and $60ton\;ha^{-1}$, and 0, 90, 180 and $270kg\;ha^{-1}$, respectively. Significantly higher dry matter yield of orchardgrass obtained were ranges of $8.92{\sim}9.70ton\;ha-1$ at levels of $180{\sim}270kg\;ha^{-1}\;yr^{-1}$ than that of other levels of mineral nitrogen. Relative yield of each cut to annual dry matter yield were 32.0% 49.2% and 18.8% for 1st cut, 2nd cut and 3rd cut in mineral nitrogen treatment. Significantly higher dry matter yield of orchardgrass obtained were ranges of $8.04{\sim}8.90ton\;ha^{-1}$ at levels of $20{\sim}60ton\;ha^{-1}\;yr^{-1}$ than that of other levels of food waste compost. The efficiency of dry matter production to application of mineral nitrogen(kg DM $kg^{-1}$ N) were 21.2, 19.0 and 15.6kg at levels of 90, 180 and $270kg\;ha^{-1}\;yr^{-1}$, respectively. Higher efficiency of dry matter Production obtained were 27.6~20.2 kg at levels of $90{\sim}180kg\;ha^{-1}$ of mineral nitrogen applied to $20ton\;ha^{-1}$ of food waste compost, it may due to accelerated mineralization by mineral nitrogen application. Highest efficiency of dry matter production to application of food waste compost (kg DM $ton^{-1}$ FWC) obtained was 71.0 kg at level of $40ton\;ha^{-1}\;yr^{-1}$. Maximum dry matter yield of orchardgrass obtained were $9.98ton\;ha^{-1}$ at limiting level of mineral nitrogen of $358.5kg\;ha^{-1}$ and $9.12ton\;ha^{-1}$ at limiting level of food waste compost of $49.3ton\;ha^{-1}$ per annum, respectively. Ranges of $20{\sim}49.3ton\;ha^{-1}$ of food waste compost and $180{\sim}358.5kg\;ha^{-1}$ of mineral nitrogen were estimated an adequate levels for increase in dry matter production, and to maintenance for orchardgrass pastures. Application of food waste compost was affected to improve the soil characteristics.