This study was conducted to evaluate mineral content of Winter Rye, Nitrogen Balance, Soil chemical characteristics and NO,-N level in infiltration water as affected by different slurry application on the basis of N contents respectively and was arranged

This study was conducted to investigate the responses of soil properties and microbial communities to different agricultural management and soil types, including organic management in Andisols (Org-A), organic management in Non-andisols (Org-NA), conventional management in Andisols (Con-A) and conventional management in Non-andisols (Con-NA) by using a pyrosequencing approach of 16S rRNA gene amplicon in Radish farms of volcanic ash soil in Jeju island. The results showed that agricultural management systems had a little influence on the soil chemical properties but had significant influence on microbial communities. In addition, soil types had significant influences on both the soil chemical properties and microbial communities. Organic farming increased the microbial density of bacteria and biomass C compared to conventional farming, regardless of soil types. Additionally, Org-NA had the highest dehydrogenase activity among treatments, whereas no difference was found between Org-A, Con-A and Con-NA and had the highest species richness (Chao 1) and diversity (Phyrogenetic diversity). Particularly, Chao 1 and Phyrogenetic diversity were increased in organic plots by 12% and 20%, compared with conventional plots, respectively. Also, regardless of agricultural management and soil types, Proteobacteria was the most abundant bacterial phylum, accounting for 21.9-25.9% of the bacterial 16S rRNAs. The relative abundance of putative copiotroph such as Firmicutes was highest in Org-NA plot by 21.0%, as follows Con-NA (13.1%), Con-A (6.7%) and Org-A (5.1%.), respectively and those of putative oligotrophs such as Acidobacteria and Planctomycetes were higher in Con-A than those in the other plots. Furthermore, LEfSe indicated that organic system enhanced the abundance of Fumicutes, while conventional system increased the abundance of Acidobacteria, especially in Non-andisols. Correlation analysis showed that total organic carbon (TOC) and nutrient levels (e.g. available P and exchangeable K) were significantly correlated to the structure of the microbial community and microbial activity. Overall, our results showed that the continuous organic farming systems without chemical materials, as well as the soil types made by long-term environmental factors might influence on soil properties and increase microbial abundances and diversity.

Purpose - Unlike in the past, individualistic thought is more dominant than groupism where members prioritize organizations. Such changes run counter to the direction of the survival of the companies, which calls for companies to explore strategies to address thems. As one of the solutions, many people highlights social capital. However, since most studies have been conducted on the definition and characteristics of social capital, there is not enough prior factor research on the formation of social capital. So the current situation require researches on the formation of social capital. Research design, data, and methodology - To achieve the purpose, the literature and the empirical studies were combined. Deriving workplace democracy and servant leadership as factors affecting the formation of social capital through the literature, and this factors have modeled assumptions about the impact on social capital, and have established hypotheses to verify them. The survey which is conducted to verify the hypothesis and questionnaires are derived base on the variables used in the previous studies. The survey was conducted 447 respondents in Korea. Results - As a result, we found that the workplace democracy is positively functioning with the formation of social capital. It means that the democracy functions as a universal element to enhance the quality of social capital at the workplace. The evidence also shows that the positive impacts of the servant leadership on the formation of social capital. And the survey shows that groups with high level servant leadership had a higher impact on the formation of social capital than those with low levels leadership. Conclusions – At present, the social capital has become an important factor for the companies pursuing high performance workplaces. We found that the workplace democracy and the servant leadership affect the formation of social capital. It means that to increase the employees’ sense of community and solidarity, it is need to form democratic environment with the servant leadership. Therefore, based on the results of this study, the workplace democracy and the servant leadership can present strategic implications that can increase the social capital.

본 연구는 제주지역 화산회토 감귤원에서 두과피복작물인 헤어리베치(Vicia villosa Roth) 의 이용 가능성을 진단하고 효율적인 양분관리 체계를 정립하기 위하여 수행하였다. 시험 은 감귤원 재배지 고도별 5개소(해발고도:신촌 37 m, 호근 116 m, 와산 123 m, 상예 161 m, 그리고 용강 232 m)에서 수행하였다. 헤어리베치 품종은 국내에서 개발된 ‘청풍보라’로 하였으며, 파종량은 ha당 30, 60 및 90 kg을 파종하였다. 시험결과 헤어리베치 입모율은 53.0~57.1%로 파종량과 고도별 포장에 관계없이 유사하였다. 파종량에 따른 잡초 발생비율 은 5개소 평균 11.8, 3.8 및 5.1%로 처리간 유의성이 없었으나 30 kg 파종구에서 다소 높은 경향을 보였으며 60 kg 및 90 kg 파종구는 각각 96.2% 및 94.9% 정도의 잡초 경감효과를 나타냈다. 헤어리베치 파종량에 따른 ha당 건물 수량은 각각 7.37, 8.43 및 8.47톤으로 30 kg 대비 60 및 90 kg 파종 시 각각 14% 및 15% 높았으나 파종량별 유의성은 없었다. 질소 수 량은 ha당 최소 175 kg (와산 30 kg ․ ha-1 파종구)에서 최대 467 kg (용강 30 kg ․ ha-1 파종구) 값을 얻었으며 파종량에 따른 5개소 평균 질소 수량은 각각 254, 316 및 315 kg으로 60과 90 kg 파종구간 차이는 없었으며, 30 kg 파종구에 비하여 24% 높았다. 감귤원에서 기상과 토양 화학성 등 재배환경 요인들이 헤어리베치 수량에 미치는 영향을 구명하기 위하여 요 인들 간 상관관계를 분석한 결과 일평균기온(R=0.2746) 및 적산온도(R=0.2714) 등 기상요인 은 헤어리베치 건물 수량에 다소 영향을 줄 수는 있으나 그 영향이 크지 않은 것으로 판단 되었다. 반면에 토양 EC (R=0.4520**), 치환성칼륨(R=0.4078**) 및 유효인산(R=0.2737) 함량 등이 높을수록 건물 수량이 증가하는 비교적 강한 양의 상관관계를 보여 기상요인 보다는 토양 화학성이 헤어리베치 수량에 미치는 영향이 큰 것으로 판단되었다. 따라서 헤어리베 치 재배시 질소 수량은 포장별 여러 가지 재배적 환경요인들의 영향을 받을 수 있으므로 포장별 일정면적의 생초 수량(X)을 측정한 후 이에 따른 질소 수량(Y)을 산출하여 활용하 는 것이 바람직할 것으로 보이며 그 산출식은 ｢Y=4.4097X+33.594 (R=0.9547)｣와 같다.

Based on the X-ray powder diffraction (XRD) and M ssbauer spectroscopy, the thermal behavior and phase transformations of two clays are investigated for raw and fired conditions, which are collected from Kwangryeongli and Ildo district in Cheju Island. M ssbauer spectra at room temperature and 20for two clays show that paramagnetic Fe3- is the structural iron of the layer silicate and ferrihydrite, and superparamagnetic goethite has about 50% of total iron contents. The XRD peaks of hematite for the fired clays appear from 800℃ in Kwangryeongli clay and from 600℃ in Ildo district clay, respectively. The structural Fe2+ was completely oxidized into Fe3- at 400℃ for Kwangryeongli clay and 500℃~600℃ for Ildo district clay, respectively. The structural Fe2+ was completely oxidized into Fe3- at 400℃. For the temperature ranging from 400℃ to 700℃~800℃, two fired clays exhibit the dehydroxylation of the clay mineral. A disintegration of the clay mineral structure is observed from 700℃~800℃ to 1100℃, followed by the onset and spread of vitrification process. It is also shown that well-crystallized hematite phase is formed at the temperature higher than 1100℃ and the relative absorption area decreases, which might be related to the recrystallization of alluminosilicate matrix.