• 아시안잔디학회지
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• 제5권2호
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• pp.59-68
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• 1991

This experiment was carried out to investigate the mixing ratio of soil amending materials such as peat perlite, active carbon and zeolite for improvements of physiochemical properties of topsoil, of creeping bentgrass (Agrostis palustris var. Penncross). The results were as followed :1.Appropriate addition of soil improvement material was increased the soil porosity due to the decrease of bulk density. Over supplement of soil improvement material induced the decrease of infiltration of water into soil.2Content of organic matter was increased in treatment of peat and active carbon . Soil reaction was decreased in peat treatment, but increased in perlite, zeolite and active carbon. Exchangeable cation capacity was increased by the addition of all kinds of soil improvement materials used in this experiment.

• 한국환경농학회:학술대회논문집
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• 한국환경농학회 2011년도 30주년 정기총회 및 국제심포지엄
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• pp.188-195
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• 2011

Red lateritic soils are typically low in total organic carbon (TOC) and available phosphorus (AP) content and continuous fertilization is required to obtain desired crop yield. In this experiment, cattle manure in three forms (air-dried, composted and vermicomposted) were applied to red lateritic soil to study their effect on TOC and AP content of soil and probable mechanism of P-solubilization as affected by these treatments were also studied. Vermicompost was the most effective to solubilize insoluble P in red lateritic soil (Alfisols) as compared to other organic amendments (air-dried cattle manure and compost). The highest SPA in vermicompost-treated soil attributed to the comparatively higher concentration of all the three SPA isozymes in these soils. The maximum P-solubilization in these soils might be attributed to the highest SPA and presence of several organic acids like citric, lactic and oxalic acids in vermicompost-treated soils. Since, vermicompost application also increased TOC, mineralizable N and exchangeable K content of soil, vermicompost could be considered as the most rational organic amendment to improve chemical properties of red lateritic soils.

• 한국토양비료학회지
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• 제6권4호
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• pp.227-230
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• 1973

C/N비(比)가 11정도(程度)로 낮은 유기물(有機物)을 다량(多量)(약(約)60%) 함유하는 한 구르타민산발효(酸醱酵) 잔사(殘渣) 가공물(加工物)과 C/N비(比)가 약(約) 22인 완숙퇴비(完熟堆肥)를 토양(土壤)에 시용(施用)하고 토양유기물(土壤有機物), C.E.C 삼상비(三相比), 입단발달등(粒團發達等)을 조사(調査)했든바 1. 토양중(土壤中) 유기물(有機物), Humic acid, Fulvic acid의 함량(含量)과 C.E.C를 증대(增大)시킴에 있어서 구르타민산발효잔사가공물(酸醱酵殘渣加工物)이 퇴비(堆肥)보다 더효과적이었다. 2. 퇴비(堆肥)와 구르타민산발효(酸醱酵) 잔사가공물(殘渣加工物)의 시용(施用)은 토양(土壤)공극율을 높였으며 전자(前者)는 기상분포비(氣相分布比)를 후자(後者)는 액상분포비(液相分布比)를 높였다. 3. 유기물(有機物)의 시용(施用)은 유효토양입단(有效土壤粒團)을 발달(發達)시켰으며 특(特)히 구르타민산발효잔사구(酸醱酵殘渣區)에서는 대입단(大粒團)(2mm 이상(以上))의 발달(發達)이 많았다.

• 한국습지학회지
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• 제16권3호
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• pp.315-325
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• 2014

월악산국립공원에 발달되어 있는 신갈나무림에서 2012년 5월부터 2013년 4월까지 유기탄소 분포와 순환을 통한 생태계 서비스 가치를 파악하였다. 지상부와 지하부 생물량에 분포되어 있는 유기탄소량은 각각 81.94 및 20.53 ton C/ha 이었으며, 낙엽층과 토양의 유기탄소량은 각각 6.49 ton C $ha^{-1}$, 141.23 ton C $ha^{-1}$ $50cm-depth^{-1}$로 조사되였다. 조사지 신갈나무림의 전체 유기탄소량은 250.19 ton C $ha^{-1}$이었으며, 이중 41.0%가 식물체에 분포하였다. 신갈나무림의 전체 유기탄소량을 원화로 환산하면 약 527만원 $ha^{-1}$의 가치를 갖는 것으로 추정되었다. 조사기간 동안 토양호흡을 통하여 방출되는 탄소량은 7.31 ton C $ha^{-1}yr^{-1}$으로 이중 미생물호흡과 뿌리호흡을 통해 방출되는 탄소량은 각각 3.58, 3.73 ton C $ha^{-1}yr^{-1}$이었다. 유기탄소 순 생산량과 미생물호흡량의 차이로 추정했을 때 본 신갈나무림에서 연간 대기로부터 흡수하는 순 유기탄소는 1.61 ton C $ha^{-1}yr^{-1}$로서, 이를 원화로 환산하면 약 33,000원 $ha^{-1}$의 가치를 갖는 것으로 추정되었다.

• 한국습지학회지
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• 제17권4호
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• pp.332-338
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• 2015

월악산국립공원에 발달되어 있는 소나무림에서 2013년 1월부터 2013년 12월까지 유기탄소 분포와 순환을 통한 생태계 서비스 가치를 평가하였다. 지상부와 지하부 생물량에 분포되어 있는 유기탄소량은 각각 32.17 및 8.04 ton C $ha^{-1}$이었으며, 낙엽층과 토양의 유기탄소량은 각각 5.55 ton C $ha^{-1}$ 및 58.62 ton C $ha^{-1}$ 50cm-$depth^{-1}$로 조사되었다. 조사지 소나무림의 전체 유기탄소량은 104.38 ton C $ha^{-1}$이었으며, 이중 37.9%가 식물체에 분포하였다. 소나무림의 전체 유기탄소량을 원화로 환산하면 약 1,044 만원 $ha^{-1}$의 가치를 갖는 것으로 추정되었다. 조사기간 동안 토양호흡을 통하여 방출되는 탄소량은 4.44 ton C $ha^{-1}yr^{-1}$으로 이중 미생물호흡과 뿌리호흡을 통해 방출되는 탄소량은 각각 2.18 및 2.27 ton C $ha^{-1}yr^{-1}$이었다. 유기탄소 순 생산량과 미생물호흡량의 차이로 추정했을 때 본 소나무림에서 연간 대기로부터 흡수하는 순 유기탄소는 0.44 ton C $ha^{-1}yr^{-1}$로서, 이를 원화로 환산하면 약 44,000원 $ha^{-1}$의 가치를 갖는 것으로 추정되었다.

• 한국습지학회지
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• 제17권3호
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• pp.283-292
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• 2015

토양으로부터 방출되는 $CO_2$의 양은 전 지구적 지구 탄소 순환에서 가장 큰 방출 중 하나로 알려져 있다. 특히 토양 내 미생물의 유기물질 분해 과정에 의해 방출되는 이산화탄소의 양은 토양의 탄소 저장량을 장기적으로 결정하는 요인이 되므로 그 양을 정량화 하는 것이 필요하다. 본 연구는 토양에서 고라니의 분변이 $CO_2$ 배출에 미치는 영향을 파악하기 위해 수행하였다. 그리고 고라니의 분변이 토양의 $CO_2$ 배출에 주는 영향과 토지의 이용에 따라 변화하는 $CO_2$ flux를 정량화 하였다. 그 결과 고라니 분변 내 많은 유기물질은 토양 미생물의 활성화에 영향을 주고 그로 인해 토양의 호흡 및 토양 내 물리 화학적인 변화가 발생되어 토양의 유기물 함량이 서로 다르게 나타남을 확인할 수 있었다. 특히 4개 지역의 토양(경작지, 휴경지, 버드나무 군락, 갈대습지)의 C/N ratio와 $CO_2$ flux는 분변의 유무와 통계적으로 매우 유의미한 상관 관계를 나타냈으며(P<0.01), 분변의 영향을 받은 토양의 $CO_2$ flux는 분변의 영향을 받지 않은 토양보다 2-20배 더 높은 것으로 나타났다. 이 연구는 고라니의 분변이 토양에 주는 영향과 야생동물 분변을 이용한 토양 물질 순환 연구를 통해 육상 생태계 및 토양권의 물질 순환과 그 영향의 정도를 정량화 하였다는 점에서 큰 의의가 있는 연구이다.

• Journal of Forest and Environmental Science
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• 제30권2호
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• pp.179-188
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• 2014

This research reports the effects of shifting cultivation on soil environment collecting samples from 0-5 cm soil depth from five locations viz. at Burburichhara, Maichchari, Longadu, Sukurchhari and Muralipara in Rangamati district of Chittagong Hill Tracts (CHTs). Soil analyses showed that fungal and bacterial population, microbial respiration and active microbial biomass, maximum water holding capacity, conductivity and moisture contents were significantly (at least $p{\leq}0.05$) lower in shifting cultivated soil compared to adjacent mixed tree plantations at all the sites. On an average in soils of 5 different shifting cultivated lands fungal population was $1.33{\times}10^5$ CFU/g dry soil and bacterial population $1.80{\times}10^7$ CFU/g dry soil and in mixed plantations fungal population was $1.70{\times}10^5$ and bacterial population $2.51{\times}10^7$ CFU/g dry soil. Organic matter and exchangeable Ca and Mg contents were significantly (at least $p{\leq}0.05$) lower and bulk density significantly (at least $p{\leq}0.05$) higher in shifting cultivated land in most of the locations compared to adjacent mixed tree plantations. Ratios of microbial respiration and organic carbon as well as active microbial biomass and organic carbon were distinctly lower and pH higher at 3 locations in shifting cultivated soils compared to mixed plantations. Findings of various soil properties, therefore, suggest that shifting cultivation has deteriorating effects on soil environment.

• 한국연초학회지
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• 제12권2호
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• pp.85-90
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• 1990

Pot experiment was conducted to find out the effect of decomposing degree of rice straw on growth characteristics of flue-cured tobacco, NC82. Tobacco growth was hindered by fresh straw of rice application. Generally, it was known that if organic matter of high Carbon/Nitrogen ratio had applied in soil, there was temporary nitrogen deficiency in plant caused by soil microorganism utilized nitrogen contained organic matter. In pot experiment, it was supposed that tobacco growth hindered by fresh straw of rice application was not nitrogen deficiency by soil microorganism, but gas toxicity by fresh straw of rice application.

• Journal of Ecology and Environment
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• 제43권2호
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• pp.129-160
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• 2019

Background: Characterizing and describing soils and land use and make a suggestion for sustainable utilization of land resources in the Ethiopian Rift valley flat plain areas of Lake Chamo Sub-Basin (CSB) are essential. Objectives: To (1) characterize soils of experimental area according to World Reference Base Legend and assess the nature and extent of salinity problems; (2) characterize land use systems and their role in soil properties; and (3) identify best land use practices used for both environmental management and improve agricultural productivity. Methods: Twelve randomly collected soil samples were prepared from the above land uses into 120 composites and analyzed. Results: Organic carbon (OC) and total nitrogen (TN) were varied along different land uses and depleted from the surface soils. The soil units include Chernozems (41.67%), Kastanozems (25%), Solonchaks (16.67%), and Cambisols (16.67%). The identified land uses are annual crops (AA), perennial crops (PA), and natural forest (NF). Generally, organic carbon, total nitrogen, percentage base saturation (PBS), exchangeable (potassium, calcium, and magnesium), available phosphorus (P₂O₅), manganese, copper, and iron contents were decreased in cultivated soils. Soil salinity problem was observed in annuals. Annuals have less nutrient content compared to perennials in irrigated agriculture while it is greater in annuals under rainfed. Clay, total nitrogen, available phosphorus, and available potassium (K₂O) contents were correlated positively and highly significantly with organic carbon and electrical conductivity. Conclusion: Management practices that improve soil quality should be integrated with leguminous crops when the land is used for annual crops production.

• Journal of Ecology and Environment
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• 제38권4호
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• pp.461-476
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• 2015

Global warming has accelerated glacial retreat in the high Arctic. The exposed glacier foreland is an ideal place to study chronosequential changes in ecosystems. Although vegetation succession in the glacier forelands has been studied intensively, little is known about the microbial community structure in these environments. Therefore, this study focused on how glacial retreat influences the bacterial community structure and its relationship with soil properties. This study was conducted in the foreland of the Midtre Lovénbreen glacier in Svalbard (78.9°N). Seven soil samples of different ages were collected and analyzed for moisture content, pH, soil organic carbon and total nitrogen contents, and soil organic matter fractionation. In addition, the structure of the bacterial community was determined via pyrosequencing analysis of 16S rRNA genes. The physical and chemical properties of soil varied significantly along the distance from the glacier; with increasing distance, more amounts of clay and soil organic carbon contents were observed. In addition, Cyanobacteria, Firmicutes, and Actinobacteria were dominant in soil samples taken close to the glacier, whereas Acidobacteria were abundant further away from the glacier. Diversity indices indicated that the bacterial community changed from homogeneous to heterogeneous structure along the glacier chronosequence/distance from the glacier. Although the bacterial community structure differed on basis of the presence or absence of plants, the soil properties varied depending on soil age. These findings suggest that bacterial succession occurs over time in glacier forelands but on a timescale that is different from that of soil development.