• 한국토양비료학회지
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• 제7권3호
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• pp.185-191
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• 1974

치환성(置換性) Al 함량(含量)에 근거(根據)한 석회소요량결정방법(石灰所要量決定方法)을 우리나라 밭 토양(土壤)에 대(對)하여 검토(檢討)한 목적(目的)으로 실내(室內) 및 Pot시험(試驗)을 실시(實施)하였던 바 그 결과(結果)는 다음과 같다. 1. 공시(供試)된 반토양(土壤)의 pH는 5.0-5.4이었고 치환성(置換性) Al함량(含量)은 1.1~3.0me/100g 범위(範圍)에 있어 경작년도(耕作年度)가 오래된 토양(土壤)일수록 그 함량(含量)은 적었다. 2. 항온(恒溫) 실험결과(實驗結果)에서 광질토양(鑛質土壤)에 있어서는 치환성(置換性) Al의 100% 상당하는 당량(當量)의 중화석회량(中和石灰量) (토양별 소석회량(消石灰量) 범위(範圍)는 45~122kg/10a)으로 대부분의 Al이 중화(中和)되어 Al 중화비율(中和比率)은 평균(平均)95% 이었으나 화산회토양(火山灰土壤)에서는 200%의 중화석회량(中和石灰量)으로도 치환성(置換性) Al이 66.5% 만이 중화(中和)되어 더욱 많은 량(量)(100% 중화량(中和量)외 약(約) 3 배(倍))의 석회(石灰)를 요구(要究)하였다. 3. 광질토양(鑛質土壤)에서는 95%의 치환성(置換性) Al이 중화(中和)되었을 때 평균(平均) pH는 5.2에서 6.3으로 높아졌으며 화산회토양(火山灰土壤)에서는 치환성(置換性) Al의 200% 중화석회량가용(中和石灰量加用)으로 pH는 5.3에서 5.5로 변화(變化)되었을 뿐이었다. 4. 치환성(置換性) Al과 치환산도(置換酸度)($y_1$)의 두 측정치(測定値)(me 단위(單位)) 간(間)에는 r=0.99로서 고도(高度)의 상관관계(相關關係)가 있었으므로 치환산도(置換酸度)는 주로 치환성(置換性) Al에 기인(起因)된 것이라는 사실(事實)을 확인(確認)하였다. 5. 야산지토양(野山地土壤)인 송정통(松亭統) 표토(表土)에 콩을 재배(栽培)한 Pot시험(試驗)에서 인산흡수계수(燐酸吸收係數)의 5% 상당(相當)의 인산(燐酸)(32.1kg/10a)을 중과석(重過石)과 용성인비(熔成燐肥)로 시용(施用)했을 때 치환산도(置換酸度)를 기준한 최적석회소요량(最適石灰所要量)(me) 산출(算出)을 위(爲)한 Liming factor는 중과석(重過石) 1.132, 용성인비(熔成燐肥) 0.594이었고 작물생육(作物生育)을 위한 최적(最適) pH는 6.0 부근이었으며 최적(最適) Al의 중화비율(中和比率)은 80~90% 이었음을 보여 주었다.

• Journal of Plant Biology
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• 제12권4호
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• pp.9-18
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• 1969

In the previous paper(part III), a certian relationships between the changes of chlorinity and organic acid released from organic material were seemed to be concened to each other in saline soil suspension. Such a possibility had been a cause to take this experiments and this experiment was carried out under the treatment of organic acid crystal, oxalic acid and succinic acid, to the soil suspension(soil: water=20g:40cc) directly. The amount of organic acid treated to the suspension were related to the contents of organic material, as amount of organic acid per gram of organic material(391.76mg). The saline soil suspension were grouped and treated with the acids in order of 78.35mg(Group 1), 391.76mg(Group 2) 979.4mg(Group 3), and 1958.8mg(Group 4), respectively. Treated suspension had been incubated at room temperature and extract from suspension was used for analysis. Followings are summary of this report. 1) Changes of pH in soil suspension appeared a little increase after the treatment of organic acid until 168 hours. 2) Total acidity of soil suspension showed a variation, however, the values of total acidity appeared not to be increased or decreased during the period of experiment. 3) Sugar contents of soil suspension was increased until 168 hours after treatment. These results are similar tendency to the previous paper. 4) Addition of organic acid to soil suspension was confirmed not to be effective method for desalination from saline soil. Chlorinity of group 3 and 4 which were treated with high concentration of organic acid showed a decrease comparing to control group.

• 미생물학회지
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• 제7권1호
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• pp.29-40
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• 1969

Two kinds of organic materials, powders of Salicornia and Oryza sativa L. wre added as a source of organic matter to the suspensions of saline soils(soil : water = 1:3) to be 4 per cent of dried saline soil grams. And then, the samples were incubated at $28^{\circ}C$ to improve the decomposition of organic materials by soil microflora. Resutls of this experiment are summarized as followings : 1) The pH of soil suspension showed its highest value on the second or third week after the treatments, which were similar to those of the soil microflora. Results of this experiment are summarized as follwings : 1) The pH of soil suspension showed its highest value on the second ot third week after the treatments, which were similar to those of the soil microflora populations. 2) Salinity increased up to the second week and the highest value of it appeared in the samples which were treated with the powder of Salicornia. In general, the salinity of all samples decreased on the third week after the treatment. The fact was assumed the possibilities of desalination from saline soil by the microbial actions. 3) Soil microflora such as bacteria, actinomycetes and fungi, were determined its populations soil microflora is to act as decomposer in soil. Both of the bacteria and actinomycytes population showed in the third weak after the tratment. In general, 30-years old of saline soil contained microbial population much more than those of 5-year old of saline soil. Salicornia powder favored the increase of both the bacteria and fungal population, and Oryza sativa L. seemed to have been a great role in increase of actinomycetes. Especially, fungal population of the untreated soil suspension contained higher microbial populations more than those of the soils treated with both of the organic materials. 4) Sugar contents of soil suspesions decreased remarkably on the first week after the treatments. 5) The amount of nitrate had similar tendency to those of population changes of soil microflora. Total acidity decreased continuously and the amount of potassium showed its highest value on the third week treatment. However, the amount of phosphorus was determined to be insignificant.

• 농업과학연구
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• 제3권2호
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• pp.139-144
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• 1976

신개간지토양(新開墾地土攘)의 합리적(合理的)인 지력증진(地力增進) 개선방안(改善方案)을 구명(究明)하기 위(爲)하여 7종(種)의 토양개량방법(土壤改良方法)을 처리(處理)하고 대두(大豆)을 재배(栽培)하였던바 그결과를 요약(要約)하면 다음과 같다. 신개간지(新開墾地) 토양(土攘)에서는 pH가 낮고 유기물(有機物)과 인산(燐酸)은 물론 석회(石灰) 마그네슘등(等)의 염기가 부족(不足)하였다. 석회(石灰)와 용성인비(熔成燐肥)는 토양산도(土壤酸度)의 교정효과(校訂效果)가 컷으며 유기물(有機物)의 증가(增加)에 대해서는 퇴비(堆肥)의 효과(效果)가 가장 큰 것과 퇴비(堆肥)와 용성인비(熔成燐肥)는 토양중(土壤中)의 칼슘함량(含量)을 증가(增加)시키는 효과(效果)가 컷으며 석회(石灰) 용성인비(熔成燐肥) 퇴비(堆肥) 및 심경(深耕)모드가 토양중(土壤中)의 고토함량(苦土含量)을 현저(顯著)히 증가(增加)시켰다. 그리고 퇴비(堆肥)는 토양중(土壤中)의 가리함량(加里含量)을 증가(增加) 시키는 효과(效果)가 현저(顯著)하다. 석회용성인비(石灰熔成燐肥) 및 퇴비(堆肥)는 식물체내의 마그네슘함량(含量)의 증가(增加)에 현저(顯著)한 효과(效果)를 나타내었으며 석회(石灰) 및 용성인비(熔成燐肥)는 각각(各各) 종실중(種實重)의 증효효과(增效效果)가 컸다. 3요소(要素) 퇴비(堆肥) 및 석회시용(石灰施用)과 동시(同時)에 심경(深耕)을 실시(實施)한 구(區)에서 최고(最高)의 종실수량(種實收量)을 보였다. 종실수량(種實收量)은 토양산도(土壤酸度), 토양중(土壤中)의 유기물(有機物) 고토함량(苦土含量) 그리고 식물체내의 고토함량(苦土含量)과 현저(顯著)한 정(正)의 상관관계(相關關係)를 나타내었다.

• 한국조경학회지
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• 제27권4호
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• pp.50-58
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• 1999

This study was carried out to investigate the growth characteristics and propagation methods of L. obtusiloba as a woody landscape plant. The results are obtained as follows: L. obtusiloba was dioecious shrub and shaped with bush type. Leaves were ovate, obtuse, cordate, 7.05 cm long, 7.20 cm wide, and petiole 2.0 cm long. Flowers of L. obtusiloba were diclinous. Soil acidity ranged from pH 4.06 to 5.53 with the lowest at the Mt. Soo-Ri. Mt. Soo-Ri located near factory district, which was considered to damaged by environmental deteoration. While soil organic matter was highest at Mt. Soo-Ri, inorganic nutrients were low. L. obtusiloba grows in the area with low soil acidity and low content of inorganic. Therefore it seemed to be tolerant to air pollution. L. Obtusiloba was high seed germination rate in the plug box and its shoots were longer than seeding box and softwood cutting of L. obtusiloba showed the rooting rate of 50% at 5,000ppm on June 23. To develop a mass propagation method of Korean native L. obtusiloba through an axillary bud culture as a woody landscape plant, about 2∼3 cm shoots induced from explant were subcultured to new media contained different growth regulators. Shoots multiplied most effectively on a WPM containing 1.0 mg/l BA, producing 5.5 shoots with a shoot length of 2.5 cm per shoot explant.

• Journal of Forest and Environmental Science
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• 제37권3호
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• pp.193-205
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• 2021

The importance of forests and trees in climate change mitigation and soil nutrient cycling cannot be overemphasized. This study assessed the above-ground carbon stock of two exotic and two indigenous tree species - Gmelina arborea, Tectona grandis, Khaya grandifoliola and Nauclea diderrichii and their litter impact on soil nutrient content of an arboretum within the University of Port Harcourt, Nigeria. Data were collected from equal sample plots from the four species' compartments. Tree growth variables including total height, diameter at breast height, crown height, crown diameter and merchantable height were measured for the estimation of above-ground carbon stock. Soil samples were collected from a depth of 0-30 cm from each compartment and analyzed for particle size distribution, organic carbon, total nitrogen, available phosphorus, exchangeable bases, exchangeable acidity, cation exchange capacity, base saturation, pH, Manganese, Iron, Copper and Zinc. Analysis of Variance (ANOVA) was used to test for significant difference (p<0.05) in the carbon contents of the four species and the soil nutrient contents of the different species' compartments. Pearson correlation was used to assess the relationships between the carbon contents, growth parameters and soil parameters. The highest and lowest carbon stock per hectare was observed for G. arborea (151.52 t.ha^-1) and K. grandifoliola (45.45 t.ha^-1) respectively. Cation exchange capacity and base saturation were highest and lowest for soil under G. arborea and K. grandifoliola respectively. The pH was highest and lowest for soil under G. arborea and T. grandis respectively. Carbon stock correlated positively with dbh, crown diameter, merchantable height and Zn and negatively with base saturation. The study revealed that G. arborea and N. diderrichii can effectively be used for reforestation and afforestation programmes aimed at climate change mitigation across Nigeria. Therefore, policies to encourage and enhance their planting should be encouraged.

• 한국환경과학회지
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• 제29권4호
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• pp.395-402
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• 2020

This study was conducted to analyze seasonal variations of de-icing salt ions harvested from soils and plants according to salt damage of Pinus densiflora f. multicaulis, a evergreen conifer, on roadsides. Pinus densiflora f. multicaulis was divided into three groups referred to SD, ND, and WD (serious salt damage (SD) = 71-100%, normal salt damage (ND) = 31-70%, and weak salt damage (WD) = 0-30%) based on the degree of visible foliage damage, and measured acidity (pH), electrical conductivity(EC), and de-icing salt ions (K⁺, Ca²⁺, Na⁺, and Mg²⁺) harvested from soils and plants. The results indicated that acidity, electrical conductivity, and de-icing salt ions of soils and plants were significantly affected by seasonal variation and salt damage. In addition, a strong positive liner relationship was observed in plants between the concentration of de-icing salts and salt damage in spring, while the relationship among seasonal variation and salt damage in soil were not significant. The results from this study has important implications for the management of conifer species in relation to salinity and roadsides maintenance.

• 한국토양비료학회지
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• 제36권2호
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• pp.80-85
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• 2003

도축폐기물에 산화칼슘을 처리하여 제조된 석회처리비료의 효과를 구명하기 위하여 배추를 공시작물로 하여 생육, 식물체중 무기성분 함량, 토양의 이화학적 특성 등을 조사하였다. 배추의 생체중은 처리구간에 통계적으로 유의성 있는 차이는 없었으나, 석회처리비료를 $169kg\;10a^{-1}$ 수준으로 시용하였을 때 삼요소 비료를 처리한 대조구보다 5% 정도 증가하는 경향이었다. 식물체중 N, P, K 함량은 석회처리비료를 시용한 시험구에서 대조구에 비해 높았으나, Mg 함량은 대조구에서 높았고 Ca 함량은 대조구에서 가장 낮았다. 석회처리비료를 $169kg\;10a^{-1}$ 수준으로 처리하였을 때 토양산도 교정효과는 석회소요량으로 부산석회분말을 처리한 경우와 동일하게 나타났다. 유기성폐기물에 석회를 처리하여 제조된 석회처리비료는 토양에 유기물을 함께 공급할 수 있는 산성토양 개량제로서 활용될 수 있을 것으로 사료된다.

• 한국토양비료학회지
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• 제35권3호
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• pp.175-184
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• 2002

복숭아 주산지역인 청도, 영덕, 영천지역 60개 과원을 대상으로 토양의 화학적 특성 및 엽중 양분함량을 조사하였다. 표토의 pH는 평균 4.8정도로 비교적 낮은 편이었고, 치환성 칼슘함량은 $3.66cmol^+kg^{-1}$, 석회 요구량은 $3,970kg\;ha^{-1}$정도였다. 산간지 토양이 평야지에 비해 석회요구량이 많았고 치환성 칼륨 및 마그네슘함량이 높았으며 양토에서 석회요구량이 가장 많았고 유효붕소함량은 양토와 사양토에서 높았다. 경작년수가 증가함에 따라 심토의 유기물함량, 표토와 심토의 칼슘함량이 증가하였고 심토의 유효인산 함량은 감소하였다. 복숭아 엽중 질소와 인산함량은 적정범위에 비해 높았고 칼슘함량은 적정범위에 비해 낮았으며 유명, 창방조생등의 품종이 천홍, 선광등 nectarine 계통에 비해 칼륨함량이 높았다. 토양 유기물함량과 식물체의 칼륨함량과 정의 상관, 칼슘함량과는 부의 상관이었고 치환성 마그네슘함량과 식물체의 칼슘함량과는 부의 상관, 마그네슘함량과는 정의 상관이었다. 따라서 경북지역 복숭아 과원은 토양산도의 교정, 퇴비, 질소 및 인산질 비료의 사용을 적절히 조절할 필요가 있는 것으로 판단된다.

• 한국잡초학회지
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• 제4권2호
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• pp.135-142
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• 1984

간척지(干拓地)의 개답년차(開沓年次) 진전(進展)에 따른 합리적(合理的) 잡초방제안(雜草防除案)을 구명(究明)하기 위한 기초자료(基礎資料)를 얻을 목적(目的)으로 계화도간척지(界火島干拓地) 지표분석(指標分析)을 하였다. 결과(結果)는 다음과 같이 요약(要約)할 수 있었다. 1. 조사지(調査地)의 토양염분온도(土壤鹽分濃度)는 대부분(大部分) 0.2% 이하(以下)로, pH는 5.5~6.5의 범위(範圍)로 변동(變動)되어 있었다. 2. 조사지(調査地)의 발생초종(發生草種)은 17종(種)으로서 매자기가 우점(優占)하고 있었으나 숙답화(熟畓化)와 함께 물달개비 쇠털골 알방동산이 등의 출현(出現)이 증가(增加)하는 경향(傾向)이었다. 3. 염온도(鹽溫度)가 낮아지고 pH가 5.5~6.5 범위(範圍)로 가까워질수록 발생초종수(發生草種數), 발생본수(發生本數), Biomass, 종다양도(種多樣度), 균재도(均在度), Sociability index가 커지는 반면에 군락특이도(群落特異度)는 작아지는 경향(傾向)이 있다. 4. 숙답화(熟沓化)가 진전(進展)될수록 온도잡초(溫度雜草), 다년생사초과(多年生莎草科), 근경횡주형(根 莖橫走型)의 잡초종(雜草種)이 줄고 일년생광엽잡초(一年生廣葉雜草)로서 풍수전파형(風水傳播型) 단립형(單立型)의 잡초종(雜草種)이 늘어가는 경향(傾向)이었다. 5. 숙답화(熟畓化)에 따른 잡초종(雜草種)의 천이(遷移) 다양화(多樣化) 다량화(多量化)가 예상되며 이에 대한 식생수준(植生水準) 및 유입전파(流入傳播)의 예방 대책이 요구(要求)될 것으로 판단(判斷)되었다.