2010년 경기도 양평군 자연리에서 발생한 땅밀림 지역의 활동연약대 부근 토양 물리적 특성을 파악하기 위해 토양분석을 실시하였다. 우리나라 산지는 기반암 상부의 표토층이 두텁지 않으므로 강우가 계속되면 물이 사면에 집중포화되어 점차 하부로 미끌어지기 쉽다. 급격하게 변화하는 기후로 인해 집중호우가 빈번히 발생하여 산지토사재해에 대한 관심과 경각심이 고조되고 있다. 본 연구는 산지토사재해 중 하나인 땅밀림의 물리적 특성을 파악하여 땅밀림의 선제적 대응에 대한 필요성을 제시하고자 수행하였다. 땅밀림의 평균 경사는 10.2°로 경사가 완만한 지형에서 발생하였다. 땅밀림의 활동연약대 단차지역의 상부와 하부지역을 분석한 후 과학적으로 비교하였다. 토양 삼각도를 이용하여 토양 형태를 판별한 결과, 미사토양, 점토성 모래토양, 모래토양 등으로 다양하였으며, 토양경도에 있어서 땅밀림지의 상부면의 경우 평균 18.74kgf/cm2, 하부면의 경우 평균 21.51 kgf/cm2 로 분석되었다. 땅밀림지의 상부면의 붕적토가 교란되어 경도가 낮게 형성되어 있었고, 단차로 붕괴되어 사면이 와해된 결과로 판단된다. 특히 인장균열 및 단차로 영향받은 하부 지역은 경도가 높으면서 토심이 깊게 측정되어 땅밀림에 취약한 결과를 나타내므로 단차가 발생된 활동연약대에 대해서 대책마련이 필요할 것으로 판단된다.

토석 채취 후 식생복구지의 토양 특성은 복구 식생의 생육에 중요하다. 본 연구는 토석 채취 후 식생복구지와 인접 소나무 및 굴참나무 임분을 대상으로 0∼10cm, 10∼20cm, 20∼30cm 깊이에 토양의 물리·화학적 특성을 조사하였다. 토양용적밀도와 토양 pH는 식생복구지가 소나무나 굴참나무 임분에 비해 유의적으로 높았으나(P<0.05), 유기탄소와 전질소농도는 인접 산림지에 비해 낮았다. 유효 인은 0~10cm 깊이에서 식생복구지 와 산림지 간 유의적인 차이가 없었으나, 교환성 칼슘은 식생복구지가 인접 산림지에 비해 유의적으로 높게 나타났다. 토양 유기 탄소저장량은 식생복구지가 9,896 kg C ha-1로 소나무 임분 131,368 kg C ha-1나 굴참나무 임분 154,381 kg C ha-1에 비해 유의적으로 낮았으며 질소저장량도(식 생복구지: 2,406 kg N ha-1; 소나무: 10,496 kg N ha-1; 굴참나무: 8,081 kg N ha-1) 유사한 경향을 보였다. 그러나 인, 포타슘, 마그네슘 저장량은 식생복구지와 인접 산림 간 유의적인 차이는 없었다. 한편, 칼슘저장량은 식생복구지가 8,998 kg Ca ha-1로 소나무 임분 697 kg Ca ha-1나 굴참나무 임분 660 kg Ca ha-1에 비해 유의적으로 크게 나타났다. 본 연구 결과에 따르면 토석 채취 후 식생복구지는 토양용적밀도와 토양 pH를 낮추고 유기물의 증가와 질소 시비 같은 양분관리가 필요한 것으로 나타났다.

본 연구는 국립공원 신규 탐방로 개방 전․후 초기 토양경도의 변화를 알아보기 위해 실시하였다. 연구대상지는 2018년 5월 16일에 개방된 설악산국립공원 점봉산 곰배골 신규 탐방로이며, 조사시기는 탐방로 개방 전 2018년 4월 27일과 탐방로 개방 후 2018년 6월 23일에 실시하였다. 토양경도 측정은 미국 Foresty Suppliers, Inc.사의 토양경도계를 이용하였으며, 분석은 Spss ver.23을 통해 시행하였다. 탐방로 개방에 따른 탐방로 좌․내․우측의 토양경도를 비교 한 결과, 탐방로 내의 토양경도는 개방 전 2.00±1.09kg/㎠에서 개방 후 3.72±0.70kg/㎠로 높아졌으며, 탐방로 좌측의 토양 경도는 개방 전 0.46±0.45kg/㎠에서 개방 후 0.98±0.68kg/㎠로, 탐방로 우측의 토양경도는 개방 전 0.51±0.42kg/㎠에서 개방 후 0.76±0.52kg/㎠로 나타났다. 탐방로 유형별(계곡, 사면)의 토양경도를 비교한 결과, 탐방로 좌측은 차이가 없는 것으로 나타났으나, 탐방로 내와 우측은 차이가 있는 것으로 나타났다. 탐방로의 토양경도는 계곡부와 사면부 등 지형 유형과 관계없이 탐방로 개방 후에 높아졌다. 본 연구의 시사점은 국립공원에서의 탐방 등 레크레이션 에 의한 생태적 영향 규명과 국립공원 핵심 서식지에서의 보전 관리 지표를 개발하는데 유용하게 활용될 것으로 판단된다.

본 연구에서는 작업기의 디스크 헤로우를 이송장치에 부착하여 실내실험을 통해 토양의 물리적 특성(함수율, 단위중량), 작업기의 특성(주행속도, 디스크 헤로우 간의 간격)에 따른 경운 토양의 반전율 등을 분석하고자 하며, 작업시기의 적정 토양의 물리적 상태를 확인하여 농가의 기초자료로 활용하고자 한다. 실험은 4가지 변수를 두고 진행하였다. 함수율, 작업 속도는 3가지 조건으로, 단위 중량은 일반적인 밭 흙 단위 중량 2.3kg/m3을 기준으로 높을 때와 낮을 때로 구분 지었으며, 디스크 헤로우의 간격은 30cm, 40cm로 구분하여 실험을 진행하였다. 이러한 4가지 변수를 두고 실험을 실시할 때 똑같은 조건으로 산포하기 위해 1m x 1m 면적의 프레임을 제작하여 일정하게 3회 석회가루를 산포하고, 경운작업 전․후의 석회가루 분포를 측정하여 반전율을 계산하였다. 반전율은 함수율별 분석 시 25%, 15%, 30% 순으로 측정되었고, 디스크 헤로우의 간격은 30cm 일 때가 더 높게 측정되었으며, 토양의 단위중량은 2.3kg/m3 이상일 때 더 높게 측정되었다.

The purpose of the study is to analyze the physical and chemical characteristics of soils from the forest fire burned area in Gyeongju National Park. According to the physical characteristics of soils, soil temperatures and soil moistures in reforestation area (site 2 and 3) and natural restoration area (site 4 and 5) were higher than in control area (site 1). In terms of chemical characteristics, hydrogen exponents (pH) in reforestation area and natural restoration area were higher than in control area. The rates of available phosphoric acid (P2O5) in control area and reforestation area (site 1) had high rates, but rates in reforestation area (site 2) and in natural restoration area (site 5) had low rates. The rates of accumulated organic matter (O. M.) in reforestation area and natural restoration area were lower than in control area. The percentages of total nitrogen (T. N.) were analyzed similarly in all study areas and soils from reforestation area and natural restoration area had higher cation exchange capacity (CEC) than from control area. Therefore these results determines that soils from the forest fire burned area are being restored to normal gradually.

Weeds are the major hindrance in the adoption of conservation agriculture in a rice wheat cropping system. There exists a conflict in the agronomic and soil requirements between a conventional rice production system and the following wheat crop. Puddling in the conventional rice productions system helps in controlling weeds in rice and following crops, but disturbs the soil structure resulting in poor stand establishment of the following wheat crop. This study was conducted to monitor the soil properties, weed dynamics and stand establishment of wheat grown by conventional and conservation tillage options after different rice production systems. Maximum soil bulk density and root penetration resistance was observed after a conventional flooded rice system with the lowest values in aerobic rice culture. Wheat stand establishment was impeded following flooded rice system; however this was quite better after the aerobic rice. However, after flooded rice, wheat stand establishment was improved with deep tillage. Hydropriming was better in improving the stand establishment than osmopriming. Weed biomass was highest after the aerobic rice; however it was a minimum after the flooded rice. Amongst the tillage systems in wheat, maximum weed flora was observed in zero tillage; however that was a minimum in bed sowing. Conservation agriculture may help in improving the stand establishment in rice wheat cropping system by improving soil physical properties, but weeds are still a major threat to adopting this form of agriculture.

Liquefaction-induced lateral spreading continues to be a major cause of damage to deep foundations. Currently there is a huge uncertainty associated with the maximum lateral pressures and forces applied by the liquefied soil to deep foundations. Furthermore, recent centrifuge and is shaking table tests of pile foundations indicate that the permeability of the liquefied sand is an extremely important and poorly understood factor. This article presents experimental results and analysis of one of the centrifuge tests that were conducted at the 150 g-ton RPI centrifuge to investigate the effect of soil permeability in the response of single piles and pile groups to lateral spreading.

This study was carried out in order to produce useful material for the forest multiple use and forest protection by soil physico-chemical analysis of studied area in Mt. Palgong. The results of soil physico-chemical analysis and statistical analysis represented as following 2 points. 1. Soil depth was in the range of average 61.1 cm and soil texture was loamy sand and sandy loam except Donghwasa area. The part of solid phase and gaseous phase were higher than other areas, but liquid phase was less in verse. Soil water content was in an average 49.5%, penetrability was average and the average of soil hardness was . This data showed that soil water content, penetrability and soil hardness were good at Mt. Palgong forest soils. 2. Soil pH was the range of 3.4 to 6.0, organic carbon content was 2.8% that is nearly mean of the Korea brown forest soils, total N content is somewhat smaller than that of other places, and total average C/N ratios was 13.9. Average available concentration was 5.05 mg/kg that is lower than that of any others. The concentration of available P of coniferous forests is higher than that of deciduous forests. Exchangeable cations content is similar to those of the Korea brown forest soil and the order of the cation content extent is > > > .

A trial was carried out to investigate the effect of fermented saw-dust pig manure (FSP) and N fertilizer application on physical, chemical properties and microbial population of soil on Cheju brown volcanic ash pasture during the period from September, 1

강원도 고성군 죽왕면과 토성면 일대의 소나무군락을 대상으로 1996년 4월에 발생한 산화에 따른 산림환경변화가 토양의 이화학성에 미치는 영향을 구명하기 위하여 비산화지역(NF) 산화후 비벌채지역(FNC), 산화후 벌채지역(FC) 및 산화후 조림지역(FCP)으로 분류하여 토양의 특성을 분석하였다. 전조사지역의 토성은 사질식양토이었고, 토양의 입경조성을 비교하면 비산화지역은 표토의 모래함량이 심토보다 낮았고, 점토함량은 높았지만 산화지역은 모두 표토의 모래함량이 점토에 비해 높았다. 토양공극 분포 중 전공극량은 지역별로 큰 차이가 없었으나, 조공극량과 투수성은 비산화지역 ＞ 산화후 비벌채지역 ＞ 산화후 조림지역 ＞ 산화후 벌채지역 순이었고, 세공극량과 가비중은 반대의 경향을 나타내었다. 이는 산화에 따른 산림환경변화로 지피식생이 제거되어 토양침식이 가속화되면서 토양 내 수분함유능력의 지표인 토양공극과 투수성에 큰 영향을 주면서 토양물리성을 악화시키고 있는 것으로 판단된다. 토양 pH는 비산화지역과 산화후 비벌채지역이 산화후 벌채지역과 조림지역보다 표토 및 심토 모두 높게 나타났다. 유기물함량 및 전질소함량 변화는 표토와 심토 모두 비산화지역＞ 산화후 비벌채지역＞ 산화후 조림지역＞ 산화후 벌채지역 순이었다. 양이온치환용량 및 치환성 양이온(K+ , Na+ /, Ca2+, Mg2+)함량 변화는 모두 표토가 심토보다 높았으며, 지역별로는 비산화지역＞ 산화후 비벌채지역＞ 산화후 조림지역＞ 산화후 벌채지역 순으로, 이는 산화후 표토층의 침식으로 지력이 악화된 결과로 사료된다.

This study was carried out to investigate the effect of no-tillage on sequential cropping supported from recycling of first crop ridge on the productivity of crop and physical properties of soil under green house condition. This study is a part of “No-tillage agriculture of Korea-type on recycled ridge”. From results for distribution of soil particle size with time process after tillage, soil particles were composed with granular structure in both tillage and no-tillage. No-tillage soil in distribution of above 2 mm soil particle increased at top soil and subsoil compared with tillage soil. Tillage and one year of no-tillage soil were not a significant difference at above 0.25 mm~below 0.5 mm, above 0.5 mm~below 1.0 mm, and above 1.0 mm of water-stable aggregate. Two years of no-tillage soil was significantly increased by 8.2%, 4.5%, and 1.7% at above 0.25 mm~below 0.5 mm, above 0.5 mm~below 1.0 mm, and above 1.0 mm of water-stable aggregate, respectively, compared with one year of no-tillage. Bulk density of top soil was 1.10 MG m3 at tillage and 1.30 MG m3 at one year of no-tillage. Bulk density of top soil was 1.14 MG m3 at two years and 1.03 MG m3 at three years of no-tillage, respectively. Bulk density of subsoil was a similar tendency. Solid phase ratio in top soil and subsoil was increased at one year of no-tillage compared with tillage soil, while soil phase ratio decreased at two and three years of no-tillage. Pore space ratio in tillage top soil (58.5%) was decreased by 8.5% at compared with no-tillage soil (51.0%). Pore space ratio was 56.9% and 61.2% at two and three years of no-tillage soil, respectively. Subsoil was a similar tendency. Gaseous phase ratio was decreased at one year of no-tillage soil, and increased at two and three years of no-tillage soil compared with tillage soil. Liquid phase ratio in top soil was increased at one year of no-tillage (28.3%), and decreased at two years (23.4%) and at three years (18.3 %) of no-tillage soil compared with tillage soil (24.2%). Subsoil was a similar tendency. Liquid phase ratio in subsoil was increased than top soil.

This study was carried out to investigate the effect of no-tillage on sequential cropping supported from recycling of first crop ridge on the growth of pepper plant and physical properties of soil under green house condition.1. Degree of crack on soil by tillage and no-tillageSoil cracks found in ridge and not found in row. At five months of tillage, crack number and crack length in length ridge were 3 and 37~51 cm in tillage. Maximum width and maximum depth in length ridge were 30 mm and 15.3cm in tillage. Crack number and crack length in width ridge were 7.5 and 7~28 cm in tillage. Maximum width and maximum depth in width ridge were 29 mm and 15.3 cm in tillage. At a year of no-tillage, crack number and crack length in length ridge were 1.0 and 140~200 cm in tillage. Maximum width and maximum depth in length ridge were 18 mm and 30 cm in a year of no-tillage. Crack number and crack length in width ridge were 11 and 6~22 cm in a year of no-tillage. Maximum width and maximum depth in width ridge were 22 mm and 18.5 cm in a year of no-tillage. Soil crack was not found at 2 years of no-tillage in sandy Jungdong series (jd) soil. Soil crack was found at 7 years of no-tillage in clayish Jisan series (ji) soil.2. Penetration resistance on soilPenetration resistance was increased significantly at no-tillage in Jungdong series (jd). Depth of cultivation layer was extended at no-tillage soil compared with tillage soil. Penetration resistance of plow pan was decreased at 1 year of no-tillage compared with than tillage soil. Penetration resistance was linearly increased with increasing soil depth at tillage in Jisan series (ji). Penetration resistance on top soil was remarkably increased and then maintained continuously at no-tillage soil.3. Drainage and moisture content of soilMoisture content of ridge in top soil was not significant difference at both tillage and no-tillage. Moisture content of ridge in 20 cm soil was 14% at no-tillage soil and 25% at tillage soil.4. Change of capacity to retain water in soilCapacity to retain water in top soil was not significant difference at 1 bar both tillage and no-tillage. Capacity to retain water in soil was slightly higher tendency in 1 year and 2 years of no-tillage soil than tillage soil. Capacity to retain water in soil was increased at 15 bar both tillage and no-tillage. Capacity to retain water in subsoil was slightly higher tendency at 1 bar and 3 bar in 2 years of no-tillage than tillage soil and a year of no-tillage soil.

This study examined the physical and chemical properties of soil in Jang-San wetland in Busan Metropolitan City. The wetland covers wide and flat area comparing to its outside. The samples of the wetland soil were collected and analyzed in order to identify the profiles and chemical properties. According to the analyses of soil moisture and particle size distribution, the wetland soil mostly belongs to sandy loam with the soil moistures of 14.9-153.2%. The soil profiles are configured with O, A, B, and C horizons from the land surface. The organic matter content (2.38-16.7%) at most sampling locations decreases downwardly with the highest at 0-20 cm depth. The organic matter content has a good positive relationship with soil moisture content. According to X-ray diffraction analysis, the wetland soils contain quartz and feldspar (the main components of rhyolite porphyry) as well as montmorillonite, gibbsite, and kaolinite (the weathered products of feldspar). The wetland soil displays the highest iron concentration (average 22,052 mg/kg), indicating oxidation of iron. High concentrations of potassium (average 17,822 mg/kg) and sodium (average 5,394 mg/kg) originate from the weathering of feldspar. Among anions, sulfate concentration is highest with average 9.21 mg/kg that may originate from sulfate minerals and atmosphere.

The purpose of this study was to identify soil physical characteristics as guideline for high yield potential inginseng cultivated field which produced 6 years root. Harvest yields of ginseng to be divided by parent rock was in order ofphyllite and red shale 3.1㎏/3.3㎡ > granite and gneiss·schist 3.0㎏ > basalt 2.6㎏ > porphyry 2.2㎏ in upland and forestsoil. Also, with classified by topography, it was in order of foot slope and alluvial fan 3.2㎏/3.3㎡ > valley 3.0㎏ > low hill2.9㎏ > hill, lave flow and dilluvial terrace 2.8㎏ in survey tilth. Class determination of soil texture, it was in order of sandyloam 3.1㎏/3.3㎡ > loam and silt loam 3.0㎏ > clay loam 2.9㎏ > silt clay loam 2.8㎏ in survey tilth. Slope condition offarming land, in case of sloping (2~7%), it was 3.1㎏/3.3㎡ but deep sloping (15~30%) caused decreasing harvest yield. Indrainage classes (excessively, well and moderately well), there was no significantly different in harvest yields. Relationshipbetween harvest yield and soil series, Production sites as yielding 3.0㎏/3.3㎡ were seven sites, also it was contained 14 soilseries. Production sites as yielding 2.5~3.0㎏/3.3㎡ were eleven sites, it was contained 16 soil series. Production sites asyielding 2.0~2.5㎏/3.3㎡ were 10 sites, it was contained 4 soil series.

The development of a new type of soil-cement concrete pavement using volcaniclastic is the main purpose of this study. Various mixture ratios, specimens' penetration resistance, time of setting, slump flow of fleshly mixed concrete, compressive strength and color characteristics of hardened concrete were studied. It was concluded that the optimum weight ratio of cement:volcaniclastic to produce good properties of soil-cement concrete is 1:3 and the use of volcaniclastic as main aggregate can improve the concrete surface color that is warm earth-tone road color. Therefore, commercial development for soil-cement concrete pavement using volcaniclastic is highly promising.

This study was carried out to investigate the improvement of soil physical and chemistry in black raspberry sequential field. We had used the subsoil-crusher, oriental herbal, perlite, popped rice hull, burned charcoal of rice hull and peat moss as a soil conditioner. On the whole, the physical and chemistry properties of treated-plots was higher than those of Control field after applying soil conditioners. Before planting, the pH and E.C. range of field was 4.9~5 and 0.5~0.6 ds/m, respectively. After applying soil conditioners, the pH and E.C range of Control field was altered to 4.3 and 2.2ds/m and the pH and E.C range of peat moss-field was 5.2 and 1.3 ds/m. The significant difference(p<0.05) in pH and E.C value was observed between Control-field and peat moss-field. In the size of soil aggregate structure, the aggregate structure weight of Control over 4mm long was 44 g and treatments of perlite, popped rice hull, burned charcoal of rice hull and peat moss was 53 g, 65g, 65g and 72g, respectively. There is a significant difference(p<0.05, 0.001) between Control and treatments. In the results of chlorophyll analysis, all of the treated-plots except for the oriental herbal have a high chlorophyll value (p<0.05, 0.001) compared to the Control. In view of the results so far achieved, there is a great difference on the frequency of dead plant between Control and treatments. The dead plants number of Control, subsoil-crusher, oriental herbal, perlite, popped rice hull, burned charcoal of rice hull and peat moss was 31, 21, 7, 12, 10, 12 and 2, respectively.

보리 후작 평야지 논에서 콩 안전 재배기술을 확립코자 보릿짚 시용 후 무경운, 경운로타리 등 경운방법을 달리하여 시험한 결과는 다음과 같다. 1. 보릿짚 시용으로 경운 유무에 관계없이 토양 중 유기물함량, 총질소, 인산 및 치환성 양이온 등이 증가하였다. 2. 토양물리성 중 공극과 토양수분함량은 경운로타리 > 로타리 > 경운로타리 후 보릿짚피복 >보릿짚소각 후 경운로타리 > 무경운 순으로 높았다. 3. 보릿짚 분해율은 파종후 30일째까지 빨랐고 그 이후는 서서히 분해되었으며, 얕게 매몰된 무경운이 경운로타리보다 빨리 분해되었고, 잡초발생량은 무경운과 보릿짚 피복에서 관행대비 각각 36%, 40% 억제되었다. 4. 콩의 뿌리활력과 근류형성능 및 콩 개화기의 생육은 무경운에서 가장 높은 값을 보였고 보릿짚 시용 후 경운로타리에서 낮은 값을 보였다. 5. 수량은 볏짚시용 후 무경운 처리에서 3,070 kg/ha으로 보릿짚 소각한 관행에 비하여 19% 증수되었으나 경운로타리는 관행수준이 었다. 따라서 평야지 논에서 콩 재배시 강우가 잦을 경우 보릿짚 시용 후 경운로타리는 토양과습을 더욱 조장하므로 무경운 골 작조 후 재배함이 가장 적절하다고 판단된다.

고추냉이 물재배에서 토양의 배지조성이 고추냉이의 생육 및 수량에 미치는 영향을 구명하기 위해 시험한 결과 토양의 입경 조성은 일본에 비하여 마사토, 강모래에서는 2mm 이상의 자갈 함량이 적었고 조사의 분포가 많았다. 토양경도는 마사토와 강모래에서 상층은 11.3~12.9, 하층은 12.5~15.1 사이에 분포하였으나, 난석에서 상층은 5.5~5.8, 하층은 6.2~7.0 사이에 분포하여 난석의 경도가 가장 낮았다. 근계 분포는 경도가 낮은 난석에서는 좁고 깊게 분포하였으나, 경도가 높은 마사토, 강모래에서는 넓고 말게 분포하였다. 근경중은 난석에서 입수구 쪽은 766kg/10a, 퇴수구 쪽은 649kg/10a, 마사토에서 입수구 쪽은 338kg/10a, 퇴수구쪽은 334kg/10a, 강모래에서 입수구 쪽은 451kg/10a, 퇴수구 쪽은 332k9/10a로 난석 대비 입수구 쪽은 마사토 44%, 강모래 59%, 퇴수구 쪽은 마사토, 강모래 각각 51% 수준이었다.

The soil from constructed wetland system for sewage treatment was analyzed to examine physical and chemical characteristics. Clogging and lowered permeability were the physical matters of concern, and nutrient and salt accumulation were the chemical matters of concern. However, the soil properties of the constructed wetland system after 3 year operation demonstrated no degradation and still the soil works almost same as the initial stage. Encouragingly, no sludge accumulation was observed inside the system. Therefore, it implies that the wetland sewage treatment system can work continuously as long as it is operated and managed properly not to cause excessive pollutant loading.

답전전환지의 잎담배 품질을 밭담배 수준으로 향상시키기 위한 재배법 개선의 기초자료로 이용 하고자 몇가지 토양개량제를 처리하여 토양의 입단형성량과 안정성등의 물리성 개선효과를 분석하고 잎담배 생육에 미친 영향을 조사한 결과는 다음과 같다. 1. 토양의 내수성 입단형성량은 polyvinylalco-hol(PVA) > perlite > zeolite순으로 많았고 식생에 적당한 크기(0.25～l.0mm)의 입단형성률은 PVA처리구에서 가장 높았다. 2. 내수성 입단형성률은 토양수분 함량이 높을 수록 입단화률도 증가하여 50%구에서 가장 높았으나 형성된 입원은 직경 2mm이상의 큰 입단비률이 높아 식생에 적당한 크기(0.25～l.00mm)의 입단형성량과 실제 농기계의 작업능률등을 고려하면 토양수분은 40%구가 적당할 것으로 판단되었다. 3. 토양립단의 안정성, 통기성 및 투수성은 토양개양제 처리로 무처리에 비해 현저히 증가되고 PVA처리구가 가장 양흐하였으며, 공린률도 무처리에 비해 다소 증가되는 경향이나 개량제종류간에는 대등하게 나타났다. 4. 토양개량제 처리로 토양 3상 비율의 개선효과가 인정되었고, 통기성은 zeolite perlite처리구가, 투수성은 PVA처리구가 높았으며, 무처리구에 비해 전체적으로 보수력이 증대되었다. 5. 연초의 생육량은 전 수량 구성요소에서 개량제처리로 현저히 증가하였고 지상부에 비해 지하부의 생장량 증가가 더 크게 나타났으며, 생장양과 연계한 토양개량제의 물리성 개선효과는 PVA > perlite > zeolite순으로 나타났다.