• 한국토양비료학회지
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• 제48권5호
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• pp.528-534
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• 2015

Green manure crops have been well recognized as the alternative for chemical fertilizer, especially N fertilizer, because of its positive effect on soil and the environment. Hairy vetch and green barley are the most popular crops for cultivation of rice in paddy field. This study was conducted to evaluate effects of hairy vetch and green barley on soil microbial community and chemical properties during short-term application (three years). For this study, treatments were composed of hairy vetch (Hv), green barley (Gb), hairy vetch + green barley (Hv+Gb), and chemical fertilizer without green manure crops (Con.). Hv+Gb treatment showed the highest microbial biomass among treatments. Principal component analysis (PCA) showed that PC1 (73.0 %) was affected by microbial biomass and PC2 (21.5 %) was affected by fungi, cy19:0/18:$1{\omega}7c$ (stress indicator). Combined treatment with hairy vetch and green barley could be more efficient than green manure crop treatment as well as chemical fertilizer treatment for improvement of soil microorganisms.

• Proceedings of the National Institute of Ecology of the Republic of Korea
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• 제4권2호
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• pp.86-94
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• 2023

Climate change is more rapid in the Arctic than elsewhere in the world, and increased precipitation and warming are expected cause changes in biogeochemical processes due to altered microbial communities and activities. It is crucial to investigate microbial responses to climate change to understand changes in carbon and nitrogen dynamics. We investigated the effects of increased temperature and precipitation on microbial biomass and community structure in dry tundra using two depths of soil samples (organic and mineral layers) under four treatments (control, warming, increased precipitation, and warming with increased precipitation) during the growing season (June-September) in Cambridge Bay, Canada (69°N, 105°W). A phospholipid fatty acid (PLFA) analysis method was applied to detect active microorganisms and distinguish major functional groups (e.g., fungi and bacteria) with different roles in organic matter decomposition. The soil layers featured different biomass and community structure; ratios of fungal/bacterial and gram-positive/-negative bacteria were higher in the mineral layer, possibly connected to low substrate quality. Increased temperature and precipitation had no effect in either layer, possibly due to the relatively short treatment period (seven years) or the ecosystem type. Mostly, sampling times did not affect PLFAs in the organic layer, but June mineral soil samples showed higher contents of total PLFAs and PLFA biomarkers for bacteria and fungi than those in other months. Despite the lack of response found in this investigation, long-term monitoring of these communities should be maintained because of the slow response times of vegetation and other parameters in high-Arctic ecosystems.

• The Korean Journal of Ecology
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• 제18권2호
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• pp.285-293
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• 1995

The relationships among the contents of Pb, Zn, Cd, Cu and microbial biomass and activity of soil were investigated in Kyongbu, Yongdong, and Chungbu highways. The heavy metal concentrations were the highest in Kyongbu highway with high traffic density. The levels of these metals in soil in three highway sites were much higher than Mt. Kwank as control site. The highest concentrations of heavy metals were found in the upper layer of soil adjacent to the roadside. Dehydrogenase activity (DHA) and adenosine tri-phosphate (ATP) contents were generally lowest at distance of 0.5 m from the roadside. Simple regression analysis indicated that DHA and ATP contents were highly negatively correlated with Pb and Zn concentrations.

• 한국토양비료학회지
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• 제42권4호
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• pp.257-265
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• 2009

토양미생물 군락에 대한 유기물 및 비료의 장기 연용 효과를 평가하고자 동일비료연용 논토양을 대상으로 미생물상, 미생물체량 및 세균 군락의 상호관계에 대해 조사하였다. 유기태 탄소함량은 비료를 연용한 곳 보다 볏짚 퇴비를 시용한 처리구에서 높았다. 토양 세균수는 무비구와 화학비료 시용구에 비해 퇴비, 석회, 규산을 병용한 처리구에서 비교적 높았다. 영년동일 논토양에서 Dactylosporangium, Ewingella, Geobacillus, Kocuria, Kurthia, Kytococcus, Lechevalieria, Micrococcus, Micromonospora, Paenibacillus, Pedobacter, Pseudomonas, Pseudoxanthomonas, Rhodococcus, Rothia, Sphingopyxis, Stenotrophomonas, Variovorax 등의 세균이 분리되었으며, Arthrobacter, Kocuria, Kurhtia 및 Bacillus 등의 세균이 우점하였다. 미생물체량 및 탈수소효소 활성은 볏짚퇴비 시용구에서 가장 높았다.

• Environmental Engineering Research
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• 제11권4호
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• pp.173-180
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• 2006

Autotrophic nitrogen removal and its microbial community from a laboratory scale upflow anaerobic sludge bed reactor were characterized with dynamic behavior of nitrogen removal and sequencing result of molecular technique (DNA extraction, PCR and amplification of 16S rDNA), respectively. In the experiment treating inorganic wastewater, the anaerobic granular sludge from a full-scale UASB reactor treating industrial wastewater was inoculated as seed biomass. The operating results revealed that an addition of hydroxylamine would result in lithoautotrophic ammonium oxidation to nitrite/nitrate, and also hydrazine would play an important role for the success of sustainable nitrogen removal process. Total N and ammonium removal of 48% and 92% was observed, corresponding to nitrogen conversion of 0.023 g N/L-d. The reddish brown-colored granular sludge with a diameter of $1{\sim}2\;mm$ was observed at the lower part of sludge bed. The microbial characterization suggests that an anoxic ammonium oxidizer and an anoxic denitrifying autotrophic nitrifier contribute mainly to the nitrogen removal in the reactor. The results revealed the feasibility on development of high performance lithoautotrophic nitrogen removal process with its microbial granulation.

• 한국유기농업학회지
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• 제23권4호
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• pp.767-779
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• 2015

본 연구에서는 신규 개간지 유기농경지에서 가축분퇴비와 녹비작물을 2년간 연용하였을 때 유기물에 의한 밭 토양미생물 군집에 미치는 영향을 평가하고자 수행하였다. 가축분 퇴비와 녹비를 연용한 처리구는 화학비료와 무비 처리구에 비해 유기물 함량이 증가하였다. 세균과 사상균 개체수는 유기물을 연용 할수록 유기물 처리구와 화학비료 그리고 무비 처리구간의 유의적인 차이를 나타내었다. 또한 가축분 퇴비와 녹비 연용으로 토양 미생물체량은 모든 처리구가 증가하였으며 NPK와 무비구에 비해 퇴비, 녹비 처리구에서 높게 나타났다. 유기물 연용에 의한 토양미생물 군집의 기능적 다양성 분석에서 가축분 퇴비, 녹비 처리구가 화학비료나 무비구에 비해 기질 이용도가 유의적으로 증가하였으며 유기물 처리구가 화학비료나 무비구에 비해 높은 종 다양성을 나타냈다. 그리고 주성분 분석에서 제2주성분에 의해 유기물 처리구와 그렇지 않은 화학비료, 무비구로 분리되었다.

• 한국토양비료학회지
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• 제37권3호
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• pp.165-170
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• 2004

화산회토 노지 감글원에서 청경, 초생, 부초재배 등의 표토관리 방법이 토양의 미생물밀도, 효소활성 및 microbial biomass C에 미치는 영향을 조사하였다. 1997년에 개화기인 5월과 과실비대기인 9월에 청경재배, 초생재배, 부초재배 감귤원 각각 10개소에서 토양을 채취하여 조사한 결과는 다음과 같다. 표토관리방법에 따른 토양의 화학성 차이는 없었으며 pH는 평균 4.7로 낮았다. 유기물과 질소 함량은 평균값으로 각각 140.2 및 $6g\;kg^{-1}$이었으나 조사지점에 따라 다양하였다. 감귤원 토양에서 호기성 세균은 $26,2-47.3{\times}10^6cfu\;g^{-1}$ 수준의 분포를 나타냈으며 호기성 세균속 중에는 Pseudomoras spp., 고온성 Bacillus spp., Rhizobium spp. 등이 우점하는 경향이었다. 방선균은 $1.8-84.6{\times}10^5cfu\;g^{-1}$ 수준으로 분포를 하였고 개화기에 밀도가 높았다. 사상균은 $26.4-182.1{\times}10^5cfu\;g^{-1}$ 수준의 분포를 나타냈으며 초생재배와 부초재배에서 많았다. 과실비대기에 토양 인산효소활성은 청경재배에서 $239.6{\mu}g\;PNP\;g\;soil^{-1}\;h^{-1}$, 토양 cellulase 활성은 초생재배에서 $602.6{\mu}g\;GE\;g\;soil^{-1}$\;24\;h^{-1}$로 높았다. Microbial biomass C는 부초재배에서 $256.3mg\;C\;kg\;soil^{-1}$로 가장 높았다.

• 한국토양비료학회지
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• 제35권4호
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• pp.243-252
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• 2002

토양생태계는 정량화하기 어려운 다양한 규칙이 다중적으로 조화되어 끊임없이 변하고있어 어떤 현상을 획일적으로 평가하기 어렵다. 그러나, 미생물은 환경에 대한 감수성이 빨라 토양의 생물적인 특성 변화를 가장 먼저 나타내기 때문에, 미생물은 생태계의 가변적 변동상의 지표가 될 수 있다. 또한 토양에 생명력을 부여해주는 기능을 가지고 있어 토양미생물의 작용 및 기능 평가는 토양 건전성 관리에 있어 중요한 역할을 한다. 따라서 본 연구는 생물학적 토양 건전성 평가 지표요인 개발하고자 주요 모재별 미경지 토양의 생물학적 토양특성을 평가하고자 수행하였다. 주요 모재별 미경지 토양의 미생물 밀도는 현무암유래 토양에서 낮고 석회암유래 토양에서 높은 경향이었으나, 그람 음성균은 비슷한 수준을 유지하고 있었다. 토양 건조처리시 미생물의 생존율은 형광성 Pseudomonas속이 0.1%로 가장 낮았으나 고온성 Bacillus속과 호알카리성균은 90%이상으로 높았다. 토양미생물체량과 미생물 유fo 유기탄소량 간에는 정의 상관관계를 나타냈으며, 토양 건조처리 효과는 토양별 9.7~95.0% 범위로 평균 39.8%였다. 건토를 재습윤하였을 때 중온성 Bacillus속은 원래 균수보다 높게 복원되는 토양이 많았다. 토양 pH는 미생물수 복원율에 정의 영향을 주었다. 건토의 재습윤화에 의한 토양 미생물체량 복원율은 평균 65.3%였으며, 재습윤토의 미생물체 복원량과 형광성 Pseudomonas속간에 유의한 정의 상관관계가 있었다.

• Journal of the korean society of oceanography
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• 제35권1호
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• pp.46-55
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• 2000

In order to understand the role of heterotrophic protists in the coastal waters off Inchon, abiotic and biotic factors were measured from January 1992 to February 1993. Microbial carbon biomass (mean212.9$^{\pm}$119.1 $^{\mu}$gC/1) was composed of 4.2% bacteria, 0.3% cyanobacteria, 12.l% autotrophic nanoflagellates, 6.6% heterotrophic nanoflagellates, 5.8 heterotrophic ciliates and 71.0% diatom and Mesodinium spp. The carbon biomass of heterotrophic protists (heterotrophic nanoflagellates and ciliates) was highest in October 1992 (mean 37.8$^{\pm}$22.5 $^{\mu}$gC/1), and was low in August 1992 (mean 21.2$^{\pm}$10.8 $^{\mu}$gC/1) and in February 1993 (mean 19.5$^{\pm}$6.4 $^{\mu}$gC/1). However, the contribution of heterotrophic protists to total microbial carbon biomass was higher in January 1992 and February 1993 (about 21%) when the phytoplankton was dominated by nanoplankton than in August and October (about 9%) when large diatoms occurred in large numbers. This study suggests that in Kyeonggi Bay heterotrophic protists might play a more important role as prey for zooplankton and as consumers of bacteria & small phytoplankton in less productive seasons (especially winter) than in productive seasons (autumn), and that the classic trophic pathway from diatoms through copepods to fish might be dominant nearly every season.

• 한국환경농학회지
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• 제24권3호
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• pp.238-244
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• 2005

Fertilization effects on changes in soil $CO_2$ flux and organic C in switchgrass (Panicum virgatum L.) land managed for biomass production were investigated. The mean daily soil $CO_2$ flux in the manure treatment was 5.63 g $CO_2-C\;m^{-2}\;d^{-1}$, and this was significantly higher than the mean value of 3.36 g $CO_2-C\;m^{-2}\;d^{-1}$ in the control. The mean daily $CO_2$ fluxes in N and P fertilizer treatments plots were not different when compared to the value in the control plots. Potentially mineralizable C (PMC), soil microbial biomass C (SMBC), and particulate organic C (POC) were highest at the 0 to 10 cm depth of the manure treatment. Potentially mineralizable C had the strongest correlation with SMBC (r = 0.91) and POC (r = 0.84). There was also a strong correlation between SMBC and POC (r = 0.90). Our results indicated that for the N and P levels studied, fertilization had no impact on temporal changes in soil organic C, but manure application had a significant impact on temporal changes in soil $CO_2$ evolution and active C constituents such as PMC, SMBC, and POC.