• 제목/요약/키워드: Different soil layers

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Soil Properties Under Different Vegetation Types in Chittagong University Campus, Bangladesh

  • Akhtaruzzaman, Md.;Roy, Sajal;Mahmud, Muhammad Sher;Shormin, T.
    • Journal of Forest and Environmental Science
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    • 제36권2호
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    • pp.133-142
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    • 2020
  • Soil physical and chemical properties at three layers such as top (0-10 cm), middle (10-20 cm) and bottom (20-30 cm) layers under three different vegetation types were studied. Soil samples were collected from Acacia forest, vegetable and fallow lands of Chittagong university campus, Chittagong, Bangladesh. Results showed that sand was the dominant soil particle followed by clay and silt fractions in all soil depths under different vegetation types. Soils of fallow land showed the highest values of bulk density while forest soils had the lowest values at three depths. Acacia forest soil having lowest values of dispersion ratio (DR) is less vulnerable while fallow soil with highest DR values is more vulnerable to soil erosion. The lower pH value at all soil layers in three ecosystems represented that soils under study are acidic in nature. Contents of organic matter, total nitrogen, exchangeable cations (Ca2+, Mg2+, K+ and Na+) and cation exchange capacity (CEC) were observed higher in Acacia forest soils compared to vegetable and fallow soils. Only soils of vegetable land had higher level of available phosphorus in three layers than that of other two land covers. The study also revealed that different soil properties were observed in three different vegetation types might be due to variation in vegetation and agronomic practices.

잣나무림에서의 시기별 토층별 토양수분 특성분석 (Analysis of Soil Moisture Characteristics in Nut Pine Forest about Seasons and Soil Layers)

  • 홍은미;최진용;유승환;남원호
    • 한국농공학회논문집
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    • 제54권4호
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    • pp.105-114
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    • 2012
  • Soil moisture plays a pivotal role in hydrological processes, especially in the forest which covers more than 64% of the national land. Soil moisture was monitored to analyze soil moisture change characteristics in terms of time and soil layers in this study. 2 Years soil moisture change data was obtained from the experimental nut pine forest and statistical analysis including auto-correlation and cross-corelation among soil moisture data from different soil layers was conducted. Using the monitored soil moisture data, a relationship between soil moisture change and precipitation was analyzed and seasonal soil moisture change characteristics were analyzed. From the result of inter-relationships among soil layers in terms of season and time lag, soil moisture change characteristics in the nut pine forest were upper soil layers were much sensitive than lowers, and seasonal variation if soil moisture for upper soil layers were bigger than lowers showing low correlation with precipitation in winter and spring due to freezing and snowfalls.

Soil properties and molecular compositions of soil organic matter in four different Arctic regions

  • Sujeong, Jeong;Sungjin, Nam;Ji Young, Jung
    • Journal of Ecology and Environment
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    • 제46권4호
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    • pp.282-291
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    • 2022
  • Background: The Arctic permafrost stores enormous amount of carbon (C), about one third of global C stocks. However, drastically increasing temperature in the Arctic makes the stable frozen C stock vulnerable to microbial decomposition. The released carbon dioxide from permafrost can cause accelerating C feedback to the atmosphere. Soil organic matter (SOM) composition would be the basic information to project the trajectory of C under rapidly changing climate. However, not many studies on SOM characterization have been done compared to quantification of SOM stocks. Thus, the purpose of our study is to determine soil properties and molecular compositions of SOM in four different Arctic regions. We collected soils in different soil layers from 1) Cambridge Bay, Canada, 2) Council, Alaska, USA, 3) Svalbard, Norway, and 4) Zackenberg, Greenland. The basic soil properties were measured, and the molecular composition of SOM was analyzed through pyrolysis-gas chromatography/mass spectrometry (py-GC/MS). Results: The Oi layer of soil in Council, Alaska showed the lowest soil pH and the highest electrical conductivity (EC) and SOM content. All soils in each site showed increasing pH and decreasing SOC and EC values with soil depth. Since the Council site was moist acidic tundra compared to other three dry tundra sites, soil properties were distinct from the others: high SOM and EC, and low pH. Through the py-GC/MS analysis, a total of 117 pyrolysis products were detected from 32 soil samples of four different Arctic soils. The first two-axis of the PCA explained 38% of sample variation. While short- and mid-hydrocarbons were associated with mineral layers, lignins and polysaccharides were linked to organic layers of Alaska and Cambridge Bay soil. Conclusions: We conclude that the py-GC/MS results separated soil samples mainly based on the origin of SOM (plants- or microbially-derived). This molecular characteristics of SOM can play a role of controlling SOM degradation to warming. Thus, it should be further investigated how the SOM molecular characteristics have impacts on SOM dynamics through additional laboratory incubation studies and microbial decomposition measurements in the field.

상수리나무림의 토양 층위별 세균군집의 계통학적 특성 (Phylogenetic characterization of bacterial populations in different layers of oak forest soil)

  • 한송이
    • 미생물학회지
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    • 제51권2호
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    • pp.133-140
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    • 2015
  • 상수리림 산림토양 각 층위 내 물리 화학적, 미생물학적 환경변수간 상관관계를 확인한 결과, 낙엽 분해 층(F)과 부식층(H)은 각 환경변수와 높은 상관관계를 갖는 특징을 나타내었다. 특히, F층에서는 pH가 C 그리고 N과 높은 상관관계를 나타내었고, 부식층(H)에서는 각종 유기산이 토양 세균 밀도와 높은 상관관계를 나타내었다. 상수리림 산림토양의 층위별 세균군집 구조의 계통해석을 위해 각 층위의 계절별 시료로부터 DNA를 직접 추출하고 DGGE 분석한 결과 낙엽층(L)의 경우 43 bands, F층은 42 bands, H층은 43 bands 그리고 근권 토양층(A)은 47 bands로 총 175 bands가 상수리림 산림토양의 DGGE 주요 bands로 선발되었다. 확보된 총 175 DGGE 주요 bands의 16S rRNA 유전자 염기서열 정보를 바탕으로 세균군집의 계통 해석한 결과, 7개 phylum에 32개 order로 세 분류되었다. 각 order에 속하는 염기서열을 heat map 분석하고 상수리림 산림토양의 각 층위을 clustering 한 결과 F층과 H층이 L층 그리고 A층과 서로 다른 cluster를 형성하는 것이 확인되었다. 또한, 산림토양의 각 층위에 존재하는 세균군집 중 약 50%가 ${\alpha}$-proteobacteria로 우점계통군으로 나타났다. 특히, Rhizobiales, Burkholderiales, 그리고 Actinobacteriales 목은 모든 계절과 모든 층위에서 보여지는 세균군집으로 확인되어 상수리림 산림토양에서 대표적인 토착세균 군집임이 확인되었다.

Interpreting in situ Soil Water Characteristics Curve under Different Paddy Soil Types Using Undisturbed Lysimeter with Soil Sensor

  • Seo, Mijin;Han, Kyunghwa;Cho, Heerae;Ok, Junghun;Zhang, Yongseon;Seo, Youngho;Jung, Kangho;Lee, Hyubsung;Kim, Gisun
    • 한국토양비료학회지
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    • 제50권5호
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    • pp.336-344
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    • 2017
  • The soil water characteristics curve (SWCC) represents the relation between soil water potential and soil water content. The shape and range of SWCC according to the relation could vary depending on soil characteristics. The objective of the study was to estimate SWCC depending on soil types and layers and to analyze the trend among them. To accomplish this goal, the unsaturated three soils were considered: silty clay loam, loam, and sandy loam soils. Weighable lysimeters were used for exactly measuring soil water content and soil water potential. Two fitting models, van Genuchten and Campbell, were applied. Two models entirely fitted well the measured SWCC, indicating low RMSE and high $R^2$ values. However, the large difference between the measured and the estimated was found at the 30 cm layer of the silty clay loam soil, and the gap was wider as soil water potential increased. In addition, the non-linear decrease of soil water content according to the increase of soil water potential tended to be more distinct in the sandy loam soil and at the 10 cm layer than in the silty clay loam soil and at the lower layers. These might be seen due to the various factors such as not only pore size distribution, but also cracks by high clay content and plow pan layers by compaction. This study clearly showed difficulty in the estimation of SWCC by such kind of factors.

Growth and yield responses of rice varieties to various soil water deficit conditions under different soil types

  • Kikuta, Mayumi;Samejima, Hiroaki;Magoti, Rahab;Kimani, John M.;Yamauchi, Akira;Makihara, Daigo
    • 한국작물학회:학술대회논문집
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    • 한국작물학회 2017년도 9th Asian Crop Science Association conference
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    • pp.322-322
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    • 2017
  • To avoid drought stress under rainfed upland conditions, it is important for rice to efficiently utilize water at shallow soil layers supplied by rainfall, and access to water retained in deer soil layers. The root developmental characteristics of rice, which play important role in the adaptability to drought conditions, vary depending on the variety. Moreover, water availability for plant differs depending on the soil types that have different physical properties such as water holding capacity, permeability, capillary force, penetration resistance, etc. In this study, we evaluated growth and yield responses of rice varieties to various soil water deficit conditions under three different soil types. The experiment was conducted in a plastic greenhouse at the Kenya Agricultural and Livestock Research Organization-Mwea from October 2016 to January 2017. Two upland varieties (NERICA 1 and 4) and one lowland variety (Komboka) were grown in handmade PVC pots (15.2 cm diameter and 85.0 cm height) filled with three different types of soil collected from major rice-growing areas of the country, namely black cotton (BC), red clay (RC), and sandy clay (SC). Three watering methods, 1) supplying water only from the soil surface (W1), 2) supplying water only from the bottom of the pots (W2), and 3) supplying water both from the soil surface and the bottom of pots (W3), were imposed from 40 days after sowing to maturity. Soil water content (SWC) at 20, 40, and 60 cm depths was measured regularly. At the harvesting stage, aboveground and root samples were collected to determine total dry weight (TDW), grain yield, and root length at 0-20, 20-40, 40-60, and 60-80 cm soil layers. Irrespective of the watering methods, the greatest root development was obtained in RC, while that in BC was less than other two soils. In BC, the degree of yield reduction under W1 was less than that in RC and SC, which could be attributed to the higher water holding capacity of BC. In RC, the growth and yield reduction observed in all varieties under W1 was attributed to the severe drought stress. On the other hand, under W2, SWC at the shallow soil depth in RC was maintained because of its higher capillary force compared with BC and SC. As the result, growths and yields in RC were not suppressed under W2. In SC, deep root development was not promoted by W2 irrespective of the varieties, which resulted in significant yield losses. Under W1, the rice growth and yield in SC was decreased although shallow root development was enhanced, and the stomatal conductance was maintained higher than RC. It was suspected that W1 caused nutrients leaching in SC because of its higher permeability. Under rainfed conditions, growth and yield of rice can be strongly affected by soil types because dynamics of soil water conditions change according to soil physical properties.

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새만금 방조제 개활지의 준설토 기반에 대한 배수층재 처리가 수목 생육에 미치는 효과 (Effects of Materials of Drainage Layer at the Reclaimed Soil Base on Tree Growth at the Open Space of Saemangeum Sea Dike)

  • 이한나;임주훈;구남인;배상원
    • 한국환경복원기술학회지
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    • 제18권1호
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    • pp.13-23
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    • 2015
  • This study was performed to compare the effects of different drainage layers on tree growth at the exposed sites of Saemangeum sea dike. 4 types of drainage layers including control(dredged soil), specially prepared bark, gravel, and wood chip were set in 150~165cm depth of soil. Pinus thunbergii and Celtis sinensis were planted after 9 months of soil treatment. Electrical conductivity(EC) of soil in all treated plots were decreased under $4dS{\cdot}m^{-1}$, and NaCl(%) was decreased under 0.05% after 1 year from soil treatment. Soil moisture at the 120cm depth of the bark treated plot was higher than that of the 180cm soil depth, below the drainage layer. It is considered that vertical mobility of water was inhibited. Organic matter(OM) at the 120cm soil depth increased at bark and wood chip treated plots. Survival rates after 4 years of P. thunbergii and C. sinensis were 100% in all treatments. The height of P. thunbergii was not significantly different among the treatments while the height of C. sinensis was significantly different among the treatments and it was highest at the bark treated plot.

인삼근부병에 관한 연구 3 (Studies on the Root Rot of Ginseng(III))

  • 이민웅
    • 미생물학회지
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    • 제12권4호
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    • pp.153-158
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    • 1974
  • Around and in the area of Wolgot-Muon, Gimpo-Gun, Kyunggi province, I examined total bacteria, general Pseudomonas spp., fluorescent Pseudomonas spp., in soil layers and also in different kinds of soil of respective diseased, uncultivated, and healthy areas, and found the followings. 1. In the diseased and uncultivated areas, the content of moisture and silt was greater than in the healthy area. 2. Contrary to the above, the healthy area contained a greater amount of inorganic elements such as $P_2O_5$, K, Ca and of soil particle such as Cs and Fs. The degree of pH and content of Mg were even in three types of soils. 3. Total bacteria were found in abundance in the healthy soil. It was observed that in all types of areas, bacteria reside in abundance in the rhizosphere, i.e., 10-15 cm layers and that the closer the surface, the greater the numbers of the bacteria. 4. General Pseudomonas spp. were also found to the greater in number on the surface of the soil, especially so in the rhizosphere, with the numbers decreasing as the soil layers increase. Numbers of this bacteria in all types of area were nearly uniform. 5. A great number of fluorescent Pseudomonas spp. were found in the diseased area, especially so in the rhizosphere.

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강변여과수 개발부지 지하수의 수리지화학적 특성 -Preliminary results

  • 현승규;우남칠;신우식;함세영
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2003년도 추계학술발표회
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    • pp.579-582
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    • 2003
  • This study is a part of the project to identify water-quality degradation mechanism due to Fe and Mn in the river-bank infiltration system in the Changwon city, Kyungsangnam-Do. Results of hydrogeochemical logging indicated that the matrix of the river bank affects groundwater quality, probably related with the hydraulic conductivities of the different layers of bank deposits. Electric conductivity logging data clearly show various layers of groundwater flows. Further studies are necessary to identify mechanisms of increasing dissolved oxygen contents with depths at some monitoring wells.

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인위적으로 변경된 토양에서의 수분보유특성 해석 모형의 적용 (Application of Analysis Models on Soil Water Retention Characteristics in Anthropogenic Soil)

  • 허승오;전상호;한경화;조희래;손연규;하상건;김정규;김남원
    • 한국토양비료학회지
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    • 제43권6호
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    • pp.823-827
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    • 2010
  • 원토양인 논토양 위에 마사토를 적토(積土)한 토양에 대한 토양수분 특성곡선을 작성해 보고, 이를 추정하는데 가장 널리 활용되고 있는 van Genuchten (VG) 모형과 Brooks-Corey (BC) 모형을 비교평가 해 그 효용성을 판단하기 위해 수행했다. 4개의 층위로 구분되는 측정 대상토양은 표토부터 30 cm 까지는 양질사토, 30~70, 70~120 cm는 사토, 120 cm 이상에서는 사양토로 분석된 토양이다. 토양수분 함량과 토양수분 메트릭 퍼텐셜과의 관계를 나타내는 토양수분 특성곡선 분석에 따르면, 원토양인 120 cm 이상 깊이 토양에서의 수분보유 특성을 제외하고 나머지 세 개 층위 토양에서의 수분 보유 특성은 0~30 cm, 30~70 cm 층위는 비슷하고 70~120 cm 층위는 약간 높은 경향이었다. 상대수분 포화도와 토양수분 메트릭 퍼텐셜의 관계를 표현함에 있어 멱함수 형태인 BC 모형보다는 해석학적 분석방법을 활용한 VG모형이 실측값에 근사한 추정결과를 제공했다. 포화상태의 종점이자 불포화상태의 시발점인 공기유입가 (AEV) 추정에도 측정 한계치 부근의 메트릭 퍼텐셜 값을 나타내는 BC모형보다는 9.5~40 cm (4 kPa)을 보였던 VG모형이 적합했다. 따라서, 인위적으로 원토양 위에 석비레 (마사토)로 적토된 토양에서의 토양수분 특성곡선 작성을 위한 추정모형에 VG모형을 활용하는 것이 바람직할 것이다. 이러한 결과로부터 VG 모형을 수자원량 산정을 위한 SCS (Soil Conservation Service, USDA) CN (Curve Number) 계산 과정에서 토양단면 내의 수분 보유 인자 (retention parameter) 산출을 위한 토양수분함량을 추정하는데 활용하거나 침투모형 (Green-Ampt Mein-Larson)을 설명하기 위한 습윤전선 매트릭 퍼텐셜을 추정하는데 사용할 수 있을 것이다.