• Current Research on Agriculture and Life Sciences
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• 제20권
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• pp.77-82
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• 2002

This study was carried out in order to produce useful material for the forest multiple use and forest protection by physico-chemical soil analysis of studied area in Sokwang-ri Forest Genetic Resource Protection Forest which was divided into in standard plots include Tricholoma matsutake and Sarcodon aspratus production forest. The result of physico-chemical soil analysis represented as following. The soil type of T. matsutake production forest was Dry brown forest soil(B1), while on the other hand the soil type of S. aspratus production forest was Moderately moist brown forest soil(B3). Between T. matsutake and S. aspratus production forest did not result in significant changes in soil pH(5.22-5.60) and soil depth(47cm), but available phosphorus, carbon, and nitrogen contents were different results. CN ratio of the fairy ring of T. matsutake was quite lower than that in S. aspratus production forests, which indicated that T. matsutake production forest was built up in the relatively immature soils which contain little organic matter. Generally, it was predicted that Pinus densiflora for. erecta forest succeeded to deciduous tree forest in stable soil environments. To conserve these T. matsutake and S. aspratus production forest, the contents of available phosphorous and exchangeable cation should be increased by continuous soil environment management and it should be established the secondary growth forests of old aged Pinus densiflora for. erecta trees as soon as possible.

• 한국식물병리학회:학술대회논문집
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• 한국식물병리학회 2003년도 정기총회 및 추계학술발표회
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• pp.91.2-92
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• 2003

In order to elucidate influence of nutritional status on rice brown spot caused by Cochliobolus miyabeanus, rice cultivation soils and rice straws were collected from paddy fields where ice brown spot occurred severely, moderately, a little and none respectively. Rice plant materials were analyzed to measure inorganic nutrients in rice straws and rice seeds. Analysis of chemical properties of rice paddy soil showed that EC and contents of available phosphate, cation and silicic acid in soil with severe infections were lower than those in healthy soil. This result suggests that amount and holding capacity of nutrient contents in soils collected from paddy field with infection of C. miyabeanus are relatively low compared to those in soils collected from healthy paddy field. Analysis of inorganic nutrients in rice straws showed that amount of macronutrient elements such as silicic acids, available phosphate and total nitrogen, and micronutrients such as copper, iron and zinc in rice straws from paddy field with infection were lower than those in healthy soil. Especially amount of iron and silicic acid were very low in rice straws from paddy field soils with infection Amount of inorganic nutrients such as iron and zinc in rice seeds was the same trend as those of rice straws. These results showed that one of major factors affecting rice brown spot was amount of nutrient contents in soil and rice straw.

• 한국산림과학회지
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• 제87권1호
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• pp.62-73
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• 1998

이 연구(硏究)는 계류수(溪流水)에서 수질평가항목(水質評價項目)의 설정시(設定時) 중요한 인자(因子)인 양(陽)이온($K^+$, $Na^+$, $Ca^{2+}$, $Mg^{2+}$)과 음(陰)이온($Cl^-$, $NO{_3}^-$, $SO{_4}^{2-}$)에 미치는 영향요인을 구명(究明)함으로써 계류수질평가기준(溪流水質評價基準)을 정립(定立)하기 위한 기초자료(基礎資料)를 제공(提供)하기 위하여 서울대학교(大學校) 농업생명과학대학(農業生命科學大學) 부속(附屬) 관악수목원내(冠岳樹木園內) 산림소유역(山林小流域)의 3개 조사구(調査區)에서 수행(遂行)하였다. 1996년 7월 1일부터 1997년 8월 31일까지 강수(降水), 수관통과우(樹冠通過雨), 토양수(土壤水) 그리고 계류수(溪流水)의 수질동태(水質動態)를 분석(分析)한 결과(結果), 계류수(溪流水)에 용존(溶存)되어 있는 $Cl^-$이온은 강수(降水)나 수관통과우(樹冠通過雨)보다는 토양수(土壤水)에 용존(溶存)되어 있는 $Cl^-$이온과 유의(有意)한 상관관계(相關關係)를 나타내었으며, 토양수(土壤水)에 용존되어 있는 $NO{_3}^-$이온은 강수(降水)에 용존되어 있는 $NO{_3}^-$이온과 유의(有意)한 상관관계(相關關係)를 나타내었다. 또한 토양(土壤) A층(層)과 B층(層)의 토양수(土壤水)에 용존되어 있는 양(陽)이온($K^+$, $Na^+$, $Ca^{2+}$, $Mg^{2+}$)과 음(陰)이온($Cl^-$, $NO{_3}^-$, $SO{_4}^{2-}$)은 통계적(統計的)으로 유의(有意)한 상관관계(相關關係)를 나타내었다. 강수(降水)에 용존(溶存)되어 있는 $NO{_3}^-$이온과 $SO{_4}^{2-}$이온의 평균농도비(平均濃度比)는 약 0.66으로 강수(降水)에는 $NO{_3}^-$이온보다는 $SO{_4}^{2-}$이온이 더 많이 함유(含有)되어 있었다. 전체 조사구에서 강수(降水), 수관통과우(樹冠通過雨), 토양수(土壤水)의 음(陰)이용량(量)은 계류수(溪流水)에 용존(溶存)하는 음(陰)이온량(量)과 유의(有意)한 상관관계(相關關係)를 나타내었으며, 강수(降水), 수관통과우(樹冠通過雨), 토양수(土壤水), 계류수(溪流水)에 용존(溶存)되어 있는 이온총량(總量)의 평균값의 크기는 토양수(土壤水)(B층(層)>A층(層))>수관통과우(樹冠通過雨)(리기다소나무림 > 벚나무림 > 서어나무림) > 계류수(溪流水) > 강수(降水)의 관계(關係)이었다.

• Applied Biological Chemistry
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• 제44권2호
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• pp.92-96
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• 2001

농경지로의 개발 가능성이 높은 중국 길림성 백성지역의 주요한 토양인 흑개토의 이화학성 및 인산 흡착특성을 조사하였다. 토지 이용방식 또는 재배작물이 서로 다른 중국 길림성 백성지역 4곳과 중국 용정에 위치한 연변 대학교 농과대학 부속 시험장 1곳에서 1993년 8월에 토양을 채취하여 실험을 수행하였다, 중국 길림성 백성지역 토양의 $_PH$는 미경작지 10.2, 경작지는 $7.3{\sim}7.6$으로 비교적 높았다. 양이온 치환용량은 20 cmol(+) $kg^{-1}$ 이상이었으며, 치환성 양이온 중 Na는 특히 표토에 많이 존재하였으며, Ca의 함량이 매우 높아 Ca 포화율이 100% 이상을 나타내었다. 토양 포화 침출액의 주요 양이온은 Na이었으며, ECe와 SAR을 기준으로 백성 미경작지 토양은 염류-나트륨성 토양, 경작지 토양은 나트륨성 또는 일반 토양에 해당하였다. 백성지역 토양의 유효인산 함량은 10mg P $kg^{-1}$ 미만으로 아주 낮았으며, 최대 인산흡착량은 $ $ mg P $kg^{-1}$이었다. 길림성 백성지역 토양의 경우 유효인산 함량이 매우 낮아 토양 비옥도 중진을 위한 인산질 비료의 시용과 함께 토양 투수성의 개선 등과 같은 적절한 토양 관리가 필요하며, 용정지역 토양의 경우에는 인산흡착 특성을 고려하여 인의 과잉 축적을 방지하기 위한 인산질 비료의 적정 시용을 권장하여야 한다.

• 한국조경학회지
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• 제27권3호
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• pp.109-113
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• 1999

The objective of this research was to develop growth media for artificial ground by blending calcined clay and coconut peat. To achieve this, aggregates of clay particles were mixed with disel oil and heated to high temperature(1150~120$0^{\circ}C$) to expand clays. The particle sizes of expanded clay were controlled to 2~5mm in diameter. Then expanded clayes were mixed with coconut peat and changes of soil physicochemical properties and their effect on plant growth of Hedera L. were determined. The infiltration rate of calcined clay was very high, but the water holding capacity, the cation exchange capacity(CEC), and the nutrient contents were low. The characteritics of coconut peat was vice verse to calcined clay. This indicates that the mixture of calcined clay and coconut peat have the better characteristics than each material. As compared to mineral soil, the infiltration rate, the water holding capacity, the CEC and the nutrient contents increased, but bulk density decreased to about 1/4. And, Hedera L. grown in the mixture of calcined clay and coconut peat(6:4, v/v) had higher plant height, longer leaf length, more total number of leaves per plant and fresh weight than that grown in mineral soil, but statistical differences were not observed between two treatments.

• 한국토양비료학회지
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• 제44권6호
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• pp.1048-1051
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• 2011

This study was carried out to find out properties and total and phytoavailable contents of heavy metals (Cd, Pb, Cu, Zn) in 21 urban agricultural soils in Seoul. The investigated urban soils showed $pH_{(1:5)}$ 6.89, $EC_{(1:5)}$ $0.14dS\;m^{-1}$, organic mater 2.22%, available $P_2O_5$ $139mg\;kg^{-1}$, cation exchange capacity (CEC) $11.36cmol_c\;kg^{-1}$, total nitrogen 0.15% and exchangeable Ca, Mg, K and Na were 6.71, 1.44, 1.06 and $0.30cmol^+\;kg^{-1}$, respectively. Total heavy metal concentrations in urban agricultural soils were lower than those of the warning levels in the area 1 according to the Soil Environmental Conservation Act of Korea. Phytoavailable-Cu, -Pb, and -Zn concentrations of the samples showed 0.02-0.28, N.D-0.09, $0.01-0.43mg\;kg^{-1}$, respectively.

• 한국토양비료학회지
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• 제33권6호
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• pp.432-445
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• 2000

본 연구는 퇴비연용 밭토양에서 유거 및 침투수에 의한 양분유실과 양분가용화정도를 구명하기 위하여 양토와 사양토를 공시하여 계분퇴비, 우분퇴비 분뇨잔사 및 식품오니퇴비등 4종을 사용하였다. 퇴비 시용량은 0, 40, $80Mg\;ha^{-1}$수준으로 처리하여 1994년부터 1997년도까지 4년간 시험한 주요 연구결과를 요약하면 다음과 같다. 퇴비종류별 양분가용회량을 조사하기 위하여 퇴비 4년연용한 토양을 배양시험한 결과 토양pH는 계분 및 우분퇴비연용은 에서 pH 6.1~6.8로 높아 졌고, 분뇨잔사시용은 pH 4.5~4.7로 무시용과 비슷하였다. 토양 EC는 배양초기에 가장 높은 후 급격히 떨어지다가 2주후부터는 일정수준을 유지하였고, 질소 무기화율은 $25^{\circ}C$조건에서 사양토는 39~76%였고 식양토는 16~48%였다. 퇴비연용토양에서 토양표면 양분 유실량은 퇴비시용량이 중가될수록 음이온이 양이온보다, 나지가 옥수수나 콩재배보다 많았다. 양이온 유실정도는 $K^+$ > $Ca^{2+}$ > $Na^+$ > $Mg^{2+}$ > $NH_4{^+}$순이었고, 음이은은 $SO_4{^{2-}}$ > $NO_3{^-}$ > $Cl^-$ > $PO_4{^{3-}}$ 순으로 많았다. 토성별 음, 양이온 지하용탈량은 사양토가 양토보다 1.7배정도 많았으며, $NO_3-N$는 퇴비 시용초기에 용탈량이 많았다. 퇴비종류별 용털량을 사양토조건의 분뇨잔사 시용구에서 제일 많게 유실되었으며, 옥수수재배는 무재배보다 58~82% 유실량이 감소되었다.

• 한국환경과학회지
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• 제10권4호
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• pp.305-310
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• 2001

pH($H_2O$), pH(KCI), CEC(cation exchange capacity), O.M.(organic matter) and exchangeable cations(K, Na, Ca, Mg) of paddy soil, upland soil and forest soil in Kumi city were investigated for the purpose of knowing soil acidification and the correlation between soil acidification and leaching of inorganic salts. The mean pH($H_2O$) values of paddy soil were 5.23(surface soil) and 5.69(subsoil) and 4.74(subsoil). The were 6.37(surface soil) and 6.11(subsoil), and those of forest soil were 4.67(surface soil) and 4.74(subsoil). The mean pH(KCl) values of paddy soil were 4.59(surface soil) and 4.98(subsoil) were 5.48(surface soil) and 5.04(subsoil), and those of forest soil were 3.82(surface soil) and 3.89(subsoil). The acidification of forest soil was more rapid than that of paddy soil and upland soil/ The total mean amounts of exchangeable cations(K, Na, Ca, Mg) in paddy soils were 6.14me/100g(surface soil) and 5.64me/100g(subsoil), and those in upland soils were 6.86me/100g(surface soil) and 6.65me/100g(subsoil), and those in forest soils were 4.06me/100g(surface soil) and 3.34me/100g(subsoil). The contents of inorganic salts in forest soil were much less than those of paddy soil and upland soil. The correlation coefficients(r) between pH($H_2O$) values and the total amounts of exchangeable cations in soils were $0.6635^{**}$(surface soil) and $0.6946^{**}$(subsoil), and those between pH(KCl) values and exchangeable cations in soils were 0.6629(surface soil) and $0.5675^{**}$(subsoil). The correlation between soil acidification and leaching of inorganic salts in soil was positively significant at 1% level.

• 한국토양비료학회지
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• 제29권2호
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• pp.199-206
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• 1996

휴경논의 증가가 쌀 생산량 감소의 원인이 됨에 따라 휴경논의 합리적 재이용을 위한 생태환경 변화 양상을 구명하기 위하여 중서부 평야 기후권에 속하는 경기도(수원 외 9)지역을 대상으로 휴경년수별로 토양특성과 식생변화를 조사한 결과는 아래와 같다. 1. 휴경논 토양의 pH, Ca, Mg 변동(變動)은 휴경기간이 길수록 심토보다 표토부분이 증가(增加)하는 경향을 나타내었다. 2. 미생물상은 휴경기간이 길수록 세균은 감소하고, 방선균은 증가 하였으나, 사상균은 변화가 작은 경향을 나타내었다. 3. 휴경논의 식생에 대한 휴경기간별 분포비율을 평균(平均)해서 비교해보면 일년생은 1년: 89.5%, 2년: 30.7%, 3년: 33.1% 다년생은 1년: 10.5%, 2년: 69.3%, 3년: 66.9%로 일년생 초종에서 급격히 다년생 초종으로 변화하였고, 초종수(草種數)도 종합하면 1년: 38종(種), 2년: 37종(種), 3년: 25종(種)으로 감소하는 경향을 보였다. 4. 휴경논에서 자라는 버드나무는 휴경기간이 길수록 본수, 직경, 초장이 증가하였으며 휴경논의 재경작시 가장 큰 문제 식생으로 생각되었다.

• 한국자원식물학회지
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• 제33권6호
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• pp.651-658
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• 2020

The aim of this study was to investigate the comparative growth characteristics and ginenoside contents of wild-simulated ginseng on different years (7 and 13-year-old) by monitoring soil properties of cultivation regions. Plant and soil samples were collected from 6 different cultivation regions. Soil organic matter (OM), total nitrogen (TN) and cation exchangeable capacity (CEC) were significantly higher in 13-year-old wild-simulated ginseng cultivation regions compared to 7-year-old wild-simulated ginseng cultivation regions. Growth characteristics of wild-simulated ginseng had shown significantly higher in 13-year-old wild-simulated ginseng compared to 7-year-old wild-simulated ginseng. Ginsenoside G-Rb1, Rb2, Rc, Rd, Re, Rf, Rg1 were significantly higher in 13-year-old wild-simulated ginseng than 7-year-old wild-simulated ginseng. According to the results of correlation analysis, soil OM, TN and CEC of the cultivated regions were positively correlated with the growth of wild-simulated ginseng. In addition, the root length of wild-simulated ginseng showed positive correlation with ginsenoside content. Hence, this study was able to investigate the correlation between growth and ginsenoside content of wild-simulated ginseng based on soil characteristics of the cultivation regions.