• Title/Summary/Keyword: 토양분류

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Microbial Changes and Yield Analysis after Soil Disinfection Treatment in Rain Shelter Greenhouse Cultivation of Gastrodia elata (천마 비가림시설 내 토양소독 처리 후 미생물상 변화 및 수량성 분석)

  • Chang Su Kim;Eun Suk Lee;Hyun Soo Jung;Jung Hyun Yoo;So Ra Choi;Young Eun Song;Sang Young Seo;Min Sil Ahn
    • Proceedings of the Plant Resources Society of Korea Conference
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    • 2023.04a
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    • pp.37-37
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    • 2023
  • 천마(天麻, Gastrodia elata Blume)는 난초과(蘭草科, Orchidaceae)에 속하는 식물로 잎과 뿌리가 없어 탄소동화능력이 없으며, 뽕나무버섯균과 공생하는 기생식물이다. 천마는 노지재배 시 혹한, 폭우 등 기상환경에 따른 연차간 수량성 차가 673~1,175kg/10a로 크고, 연작에 따른 수량성이 연작 1회 시 29%, 연작 2회 시 68%가 감소하는 경향을 보이고 있다. 최근 기후변화 대응으로 비가림시설재배가 이뤄지고 있으나, 비가림 시설재배 또한 연작장해가 발생하고 있다. 따라서, 본 연구는 비가림시설을 활용한 천마 재배의 연작장해 경감을 위해 태양열(6~10월, 비닐피복) 및 토양훈증(메탐소듐, 30 L/1,000 m2)으로 토양소독 처리를 하였고, 윤작(수단그라스)을 대조구로 설정하여 토양 화학성, 미생물상 및 수량성을 분석하였다. 토양소독 전·후 토양내 화학성을 분석한 결과, 비가림시설재배 시 토양 화학성의 변화는 거의 없었다. 토양소독 후 metagenome 분석 결과, JCR21(윤작), JCS21(태양열), JCF21(토양훈증)의 시료로부터 확보한 총 read는 598,425개였으며, 이 중에서 Eukaryota로 분류되지 않은 read는 2,397개(0.4%), no hit, not assign된 read는 17,094개 (2.9%), Bacteria로 분류된 read는 281,391개(47.0%), Eukaryota로 분류된 read는 총 297,543개(49.7%)였다. JCR21은 전체 read의 35.0%, JCS21은 34.0%, JCF21은 31.0%를 차지했고, Eukaryota는 JCR21 대비 JCS21, JCF21에서 각각 9.9%, 18.9% 낮았다. 그리고, Bacteria는 JCR21 대비 JCF21은 5.4% 감소하였으나, JCS21은 1.4% 증가하였다. 이 중 Eukaryota에서 종(species)명까지 정확하게 밝혀진 것은 27종이었고 속(genus) 으로는 18속이었다. JCF21은 전체 read의 30.2%, JCS21은 33.8%, JCR21은 36.0%를 차지했고, JCF21 포장은 토양훈증으로 JCS21에 비해 3.6%, JCR21에 비해 5.8%까지 균수가 감소함을 알 수 있었다. 대체적으로 발견된 균은 고르게 분포하고 있었으나 초작지, 연작 1회지, 연작 2회지에서는 많이 발견되지 않았던 Mucoromycota (41,490 read, 13.9%), Agaricales (10,586 read, 3.6%)가 높은 비율로 분포를 하고 있었다. 토양소독 처리에 따른 10a 당 수량을 살펴본 결과, 윤작 1,309 kg, 태양열소독 1,609 kg, 토양훈증 1,733 kg으로 나타났고, 수량지수가 윤작 처리구 대비 태양열소독은 23%, 토양훈증은 32% 높았다. 성마율은 윤작 51%, 태양열소독 63%, 토양훈증 68%으로 나타났으며, 자마율은 윤작 49%, 태양열소독 37%, 토양훈증 32%으로 나타났다. 괴경썩음 정도는 윤작 30-49%, 태양열소독 10-19%, 토양훈증 5-9%로 나타났다. 따라서, 비가림시설을 활용한 천마 재배 시 토양훈증 소독 처리를 하면 연작이 가능할 것으로 판단되었다.

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Diversity and Phylogenetic Analysis of Fluorescent Pseudomonads Isolated from Soil-Root System of Red Pepper in Greenhouse (비닐하우스 고추재배지의 토양과 근계로부터 분리된 형광성 Pseudomonads의 계통 분류 및 다양성)

  • Kwon, Soon-Wo;Kim, Jong-Shik;Song, Jae-Kyeong;Ryu, Jin-Chang
    • Korean Journal of Soil Science and Fertilizer
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    • v.33 no.4
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    • pp.275-282
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    • 2000
  • Among the fluorescent pseudomonad isolates from soil- root system of red pepper in Chinju, Kyunsangnam-Do, the phylogenetic analysis for 35 isolates were conducted. The partial 16S ribosomal DNA sequences were used as taxonomic key for phylogenetic analyses, and these sequences were enabled to identification of the fluorescent pseudomonad isolates on the species level. The 17 isolates among them were classified into Pseudomonas putida group, and consisted of the strains isolated mainly from soil. This group were subdivided into 4 subgroups (I, II, III, and IV). The subgroup I and IV were unique ones which were relatively remotely related with subgroup II and III including the type strain of P. putida. The 15 isolates among 35 isolates were grouped along with the type strain of Pseudomonas fluorescens, and 3 isolate were characterized as intermediates of P. fluorescens and Pseudomonas chlororaphis. Most of strain isolateds from the rhizosphere soil and rhizoplane of red pepper were identified as P. fluorescens and closely related with each other. In this study, root of red pepper was supposed to be colonized by a specific strain or strains of P. fluorescens.

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Topographic Characteristics, Formation and Classification of Soils Developed in Limestone -II. Clay Mineralogical Properties, Formation and Classification of Limestone Soils from Yeongweal Area of Gangweon-Do (석회암(石灰岩) 토양(土壤)의 지형적(地形的) 특성(特性)과 생성(生成) 및 분류(分類) -II. 강원도(江原道) 영월지역(靈越地域) 석회암(石灰岩) 토양(土壤)의 점토광물특성(粘土鑛物特性)과 생성(生成) 및 분류(分類))

  • Jung, Sug-Jae;Kim, Tai-Soon;Kim, Young-Ho;Moon, Joon
    • Korean Journal of Soil Science and Fertilizer
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    • v.23 no.1
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    • pp.1-7
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    • 1990
  • Clay mineralogical properties, soil formation and classification for the limestone derived soil were discussed from the 4 soil series, Pyeongchang, Anmi, Yulgog, and Mungyeong, distributed over the area of Bangjeol-Ri, Yeongweol-Eup, Gangweon-Do. The results are as follows; 1. Kaolinite and Al-interlayered vermiculite were the main clay minerals and other minerals were illite, vermiculite, and chlorite. 2. CEC of topsoil ranged from 10.5 to 22.9me/100g and that of sub-soil ranged from 10.0 to 23.8me/100g. CEC seemed to be increased with descending from topograpical position and had slightly significant positive correlation. 3. Lithologic changes as a runction of soil depth showed smooth change for Pyeongchang, discontinuity for Anmi, unpredictability for Yulgog, and uniformity for Mungyeong series. 4. According to the new system of soil taxanomy Pyeongchang series was classified as Typic Hapludalfs, Anmi as Fluventic Eutrochrepts, Yulgog as Fluvaquentic Eutrochrepts, and Mungyeong as Aeric Haplaquepts.

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Classification of hysteretic loop feature for runoff generation through a unsupervised machine learning algorithm (비지도 기계학습을 통한 유출 발생 내 이력 현상 구분)

  • Lee, Eunhyung;Jeon, Hangtak;Kim, Dahong;Friday, Bassey Bassey;Kim, Sanghyun
    • Proceedings of the Korea Water Resources Association Conference
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    • 2022.05a
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    • pp.360-360
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    • 2022
  • 토양수분과 유출 간 관계를 정량화하는 것은 수문 기작 및 유출 발생 과정의 이해를 위한 중요한 정보를 제공한다. 특히, 유출과정의 특성화는 수문 사상에 따른 불포화대 내 토양수 및 토사 손실 제어와 산사태 및 비점오염원 발생 예측을 위해 필수적이다. 유출과정과 관련된 비선형성과 복잡성을 확인하기 위해 토양수분과 유출 사이의 이력 거동이 조사되었다. 특히, 수문 과정 내 이력 현상 구체화를 위해 정성적인 시각적 분류 및 정량적 평가를 위한 이력 지수들이 개발되었다. 정성적인 시각적 분류는 시간에 따라 시계 및 반시계방향으로 다중 루프 형상을 나누는 방식으로 진행되었고, 정량적 평가의 경우 이력 고리(Hysteretic loop) 내 상승 고리(Rising limb)와 하강 고리(Falling limb)의 차이를 기준으로 한 지수로 이력 현상을 특성화하였다. 이전에 제안된 방법론들은 연구자의 판단이 들어가기 때문에 보편적이지 않고 이력 현상을 개발된 지수에 맞춤에 따라 자료 손실이 나타나는 한계가 존재한다. 자료의 손실 없이 불포화대 내 발생 가능한 대표 이력 현상을 자동으로 추출하기 위해 적합한 비지도 학습기반 기계학습 방법론의 제안이 필요하다. 우리 연구에서는 국내 산지 사면에서 강우 사상 동안 다중 깊이(10, 30, 60cm)로 56개의 토양수분 측정지점에서 확보된 토양수분 시계열 자료와 산지 사면 내 위어를 통해 확보된 유출 시계열 자료를 사용하였다. 먼저, 기존에 분류 방법을 기반으로 계절 및 공간특성에 따라 지배적으로 발생하는 토양수분-유출 간 이력 현상을 특성화하였다. 다음으로, 토양수분-유출 간 이력 패턴을 자료 손실 없이 형상화하여 자동으로 데이터베이스화하는 알고리즘을 개발하였다. 마지막으로, 비지도 학습방법을 이용하여 데이터베이스화된 실제 발현 이력 현상 내 확률분포를 최대한 가깝게 추정하는 은닉층을 반복적인 재구성 학습을 통해 구현함으로써 대표 이력 현상 패턴을 추출하였다.

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Taxonomical Classification of Namweon Series, Black Volcanic Ash Soils (흑색 화산회토인 남원통의 분류)

  • Song, Kwan-Cheol;Hyun, Byung-Geun;Sonn, Yeon-Kyu;Lim, Han-Cheol;Lee, Shin-Chan
    • Korean Journal of Soil Science and Fertilizer
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    • v.42 no.5
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    • pp.385-392
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    • 2009
  • This study was conducted to reclassify Namweon series, black volcanic ash soils, in Jeju Island based on the second edition of Soil Taxonomy : A Basic System of Soil Classification for Making and Interpreting Soil Surveys. Morphological properties of typifying pedon of Namweon series were investigated and physicochemical properties were analyzed according to Soil Survey Laboratory Methods Manual. The typifying pedon of Namweon series has black (10YR 2/1) silt loam Ap horizon (0~11 cm) and black (10YR 2/1) silt loam BA horizon (11~72 cm). Bw horizon (72~100 cm) is very dark brown (10YR 2/2) silt loam. That occurs on lava plain derived from volcanic ash materials. The typifying pedon contains 5.2~6.4% oxalate extractable (Al + 1/2 Fe), over 85% phosphate retention, and lower bulk density than $0.90Mg\;m^{-3}$. Ap, BA, and Bw horizons of the pedon have andic soil properties. That can be classified as Andisol. The typifying pedon has an udic soil moisture regime and has a 1,500 kPa water retention of 15% or more on air-dried samples throughout all horizons, and can be classified as Udand. Ap and BA horizons (0~72 cm) have a color value, moist, and chroma of 2 or less, melanic index of 1.70 or less, and 6% or more organic carbon. That meets the requirements of melanic epipedon. That keys out as Melanudand. That has more than 6.0% organic carbon and the colors of mollic epipedon throughout a layer 50 cm or more thick within 60 cm of the mineral soil surface.. Thus, that keys out as Pachic Melanudand. The pedon has a fine-earth fraction that has a water content at 1,500 kPa tension of 12% or more on air-dried samples and has less than 35% (by volume) rock fragments. Thus, the substitute for particle-size class is medial. That has a sum of 8 times the Si (percnt by weight extracted by acid oxalate) plus 2 times the Fe (percnt by weight extracted by acid oxalate) of 5 or more, and 2 times the Fe is more than 8 times the Si. Thus, the mineralogy class is ferrihydritic. Namweon series can be classified as medial, ferrihydritic, thermic family of Pachic Melanudands, not as ashy, thermic family of Typic Melanudands.

Taxonomical Classification and Genesis of Jeju Series in Jeju Island (제주도 토양인 제주통의 분류 및 생성)

  • Song, Kwan-Cheol;Hyun, Byung-Geun;Moon, Kyung-Hwan;Jeon, Seung-Jong;Lim, Han-Cheol;Lee, Shin-Chan
    • Korean Journal of Soil Science and Fertilizer
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    • v.43 no.2
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    • pp.230-236
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    • 2010
  • Jeju Island is a volanic island which is located about 96 km south of Korean Peninsula. Volcanic ejecta, and volcaniclastic materials are widespread as soil parent materials throughout the island. Soils on the island have the characteristics of typical volcanic ash soils. This study was conducted to reclassify Jeju series based on the second edition of Soil Taxonomy and to discuss the formation of Jeju series in Jeju Island. Morphological properties of typifying pedon of Jeju series were investigated, and physico-chemical properties were analyzed according to Soil survey laboratory methods manual. The typifying pedon has dark brown (10YR 3/3) silt clay loam A horizon (0~22 cm), strong brown (7.5YR 4/6) silty clay BAt horizon (22~43 cm), brown (7.5YR 4/4) silty clay Bt1 horizon (43~80 cm), brown (7.5YR 4/6) silty clay loamBt2 horizon (80~105 cm), and brown (10YR 5/4) silty clay loam Bt3 horizon (105~150 cm). It is developed in elevated lava plain, and are derived from basalt, and pyroclastic materials. The typifying pedon contains 1.3~2.1% oxalate extractable (Al + 1/2 Fe), less than 85%phosphate retention, and higher bulk density than 0.90 Mg $m^{-3}$. That can not be classified as Andisol. But it has an argillic horizon from a depth of 22 to 150 cm, and a base saturation (sum of cations) of less than 35% at 125 cm below the upper boundary of the argillic horizon. That can be classified as Ultisol, not as Andisol. Its has 0.9% or more organic carbon in the upper 15 cm of the argillic horizon, and can be classified as Humult. It dose not have fragipan, kandic horizon, sombric horizon, plinthite, etc. in the given depths, and key out as Haplohumult. A hoizon (0~22 cm) has a fine-earth fraction with both a bulk density of 1.0 Mg $cm^{-3}$ or less, and Al plus 1/2 Fe percentages (by ammonium oxalate) totaling more than 1.0. Thus, it keys out as Andic Haplohumult. It has 35% or more clay at the particle-size control section, and has thermic soil temperature regime. Jeju series can be classified as fine, mixed, themic family of Andic Haplohumults, not as ashy, thermic family of Typic Hapludands. In the western, and northern coastal areas which have a relatively dry climate in Jeju Island, non Andisols are widely distributed. Mean annual precipitation increase 110 mm, and mean annual temperature decrease $0.8^{\circ}C$ with increasing elevation of 100m. In the western, and northern mid-mountaineous areas Andisols, and non Andisols are distributed simultaneously. Jeju series distributed mainly in the western and northern mid-mountaineous areas are developed as Ultisols with Andic subgroup.