• 환경생물
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• 제27권4호
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• pp.353-362
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• 2009

This study attempted to compare the litter decomposition rate of Arundinella hirta and Miscanthus sinensis var. purpurascens which collected from serpentine soil acting potentially toxic concentration of heavy metals and non-serpentine soil by using the microcosm method for 192 days under constant humidity and $23^{\circ}C$. The contents of Ni, Fe, Mg and Cr in the serpentine and nonserpentine soil originated litter showed high differences between them. The litter samples from serpentine site have lower C/N than non-serpentine litter, but the soluble carbohydrate content was shown almost similar between two plant litter. The mass loss rates of leaf litter from serpentine area were slower than those from non-serpentine site. During the experimental period, the remained dry weight of A. hirta and M. sinensis var. purpurascens litter collected from serpentine site were 64.7%, 65.0% of initial dry weight and litter samples from non-serpentine site showed 54.2%, 50.7%, respectively. K and Na were leached rapidly at the initial decomposition periods, but Ca showed immobilization and other metal elements reserved at the decomposing litter for a long time. The decomposing A. hirta litter from non-serpentine soil showed higher values of $CO_2$ evolution, microbial biomass-C, and microbial biomass-N than those in serpentine soil originated litter acting nutrient stresses and exhibited rapid decay rate. The microbial biomass and microbial respiration of decaying litter were positively correlated with litter decomposition rate, and these relationships showed more rapid slope in non-serpentine soil originated litter than that in serpentine soil.

• 환경생물
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• 제24권4호
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• pp.408-415
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• 2006

Serpentines soil have high values of magnesium and low values of calcium, and are usually deficient in N and P, but rich in iron, Ni, silicates. We investigated serpentine soil properties and measured the content of nutrient elements and heavy metals in shoots and root of plant species which were in common at serpentine and non-serpentine areas in Andong, Korea. The soils showed higher pH value above 6.9. The contents of Ni, Cr, Fe and Mg of serpentine soils exhibited 77, 27, 5.5 and 12.5 times more than in non-serpentine soils, respectively. The content of Na was almost same but K was two times higher in non-serpentine soil, compared with serpentine soil. The contents of nutrient element such as K, Ca, Na and P in serpentine plants did not show conspicuous differences with non-serpentine plants. On the other hand, the concentrations of Ni, Cr, Fe, Mg and Mg/Ca were very high in plant on serpentine area. The all plant species collected at the serpentine site were bodenvag plants, which are not restricted to a specific type of substrate. By the plant species and parts of plant tissues, the absorption levels and patterns showed high variation and were species-specific. Carex lanceolata, Lysimachia clethroides and Cynanchum paniculatum contained much chromium and Eupatorium chinense and C. paniculatum exhibited high contents of Ni. In leaf tissue, C. lanceolata, Rubus parvifolius, Festuca ovina, Quercus serrata, and L. clethroides took comparatively large amount of Cr in serpentine area. E. chinense contained large amount of Ni, Cr and Fe in a leaf tissue. The stem of Galium verum, Juniperus rigida included high amount of Cr, Ni and Fe. And C. paniculatum absorbed large amount of Ni and Cr in the stem.

• Journal of Ecology and Environment
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• 제31권4호
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• pp.327-331
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• 2008

Serpentine soils are distributed in a small area in Korea, and generally exhibit high contents of Ni, Cr, Fe, Mn, Co and Mg. We investigated the growth of woody plants and herbs in the Andong serpentine area, Korea. Pinus densiflora and P. rigida growing on serpentine soils have high contents of Fe, Mg, Ni and Co, with contents approximately twice as high as those of non-serpentine plants. Tree species on serpentine soil also had lower ratios of tree height/DBH than trees in a control area. In greenhouse culture experiments on two bodenvag herb species, Setaria viridis and Cymbopogon tortilis, the biomass of the plants was significantly affected by soil type but not by seed origins. After 66 days, the growth of S. viridis and C. tortilis seedlings was significantly inhibited in serpentine soil, and the dry weight of each species showed significant negative correlations with soil heavy metal contents (Ni, Co and Cr). These results suggest that the growth of plants was inhibited by properties of the serpentine soil, and in particular, their high heavy metal concentration, which induced dwarfing in woody plants and reduction of total plant biomass in herbs.

• 한국환경생태학회지
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• 제24권4호
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• pp.426-435
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• 2010

본 연구는 사문암 토양의 화학적 성질과 토양미생물량 및 토양효소 등 토양의 생물학적 활성을 대조구의 비사문암 토양과 비교하고, 사문암과 비사문암에서 공통으로 서식하는 새(Arundinella hirta)와 억새(Miscanthus sinensis var. purpurascens)의 낙엽이 입지가 다른 사문암지역과 비사문암 지역에서 분해될 때 분해율의 차이가 어떻게 유발되는지 9개월 동안 야외에서 교차 실험하였다. 사문암 토양은 비사문암 토양에 비하여 높은 pH, 낮은 dehydrogenase 와 urease활성을 나타내었으며 alkaliphosphatase의 활성은 높았다. 두 토양에서 microbial biomass-C와 N의 차이는 유의하지 않았으나 사문암 토양에서 microbial biomass-N함량이 더 높게 나타나 비사문암 토양에서 보다 낮은 토양의 C/N을 나타내는 원인이 되었다. 사문암지역에서의 낙엽분해실험에서는 사문암지역에서 획득한 새와 억새 낙엽이 각각 39.8%, 38.5%의 중량감소를 보였으며, 비사문암 토양에서 획득한 낙엽은 각각 41.1%, 41.7%의 중량감소를 나타내었다. 비사문암지역에서의 낙엽분해실험에서는 사문암낙엽이 46.8%, 42.2% 그리고 비사문암낙엽은 44.8%, 37.4%의 중량감소를 각각 보였다. 이러한 결과는 중금속을 포함하는 토양의 영향보다는 낙엽의 질적 차이가 분해율에 더 큰 영향을 미쳤음을 나타내준다. 일반적으로 낮은 C/N을 갖는 낙엽이 더 빨리 분해된다는 결과와는 달리 낮은 C/N을 갖는 사문암낙엽의 분해가 느린 것은 낙엽에 포함된 중금속의 저해가 낙엽의 C/N이나 lignin/N과 같은 낙엽의 질적 차이에서 유발되는 낙엽분해의 저해보다 큰 영양을 미친다는 결과를 보여주었다. 또한 낙엽분해가 진행되는 동안 낙엽내의 Cr, Ni과 Mg, Fe의 농도는 점차 증가하였으며 이러한 경향은 사문암지역에서 현저하였다.

• 한국조경학회지
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• 제30권3호
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• pp.86-93
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• 2002

The objectives of this research were to investigate the effect of serpentine as a new soil conditioner for growth of turfgrass. To achieve the goal, pure sand or mixtures of sand and serpentine with various ratios were tested for soil physical properties and the growth effects of perennial ryegrass and zoysiagrass growth were compared. Major results of this research are summarized as follows; 1) Hydraulic conductivity of 10~30% serpentine mixtures were observed within the range of 1010~901mm/h which is good for USGA recommendation. Experimental results of pH and EC for various mixtures indicated that the 10% serpentine mixture was the most suitable for turfgrass growth. 2) Perennial ryegass treated with 10% serpentine mixture showed the highest visual quality(p<0.01) among all treatments. And serpentine treatment was more effective to improve visual quality of perennial ryegrass than that of zoysiagrass. The treatment of 10% serpentine had better visual qualities than that of 20% in both of zoysiagrass and perennial ryegrass. Treatment with the right amount of serpentine extends green period for one to two weeks during early winter in both zoysiagrass and perennial ryegrass. 3) In perennial ryegrass, the treatment of 10% serpentine resulted in an increase of total dry weight compare with those of zeolite or barley stone, and also dramatically promoted the dry weight by 15% compared with sand 100%(control). Total dry weight of zoysiagrass treated with 10% serpentine was 9％ higher than that of san. These results indicated that serpentine can be a good soil conditioner for both zoysiagrass and perennial ryegrass when it is blended with sand within a range of 10 to 20% by volume.

• 한국환경생태학회지
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• 제32권6호
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• pp.676-685
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• 2018

경북 안동 사문암 지역의 소나무군락에서 2017년 01월부터 2017년 12월까지 1년간 매목조사, 미기상 및 토양호흡 측정을 통해 탄소수지를 측정하였다. 사문암 지역에서 토양호흡량은 연중 42.48 ~ 262.61 g $CO_2{\cdot}m^{-2}{\cdot}month^{-1}$의 범위로, 평균 $151.71{\pm}75.09g$ $CO_2{\cdot}m^{-2}{\cdot}month^{-1}$로 측정되었다. 대조구인 비사문암 지역의 소나무림에서는 연중 20.94 ~ 449.24 g $CO_2{\cdot}m^{-2}{\cdot}month^{-1}$의 범위로 조사되었으며, 평균 $165.09{\pm}118.96g$ $CO_2{\cdot}m^{-2}{\cdot}month^{-1}$로 측정되었다. 사문암 지역과 비사문암 지역의 총 탄소저장량은 각각 91.90, $222.85ton{\cdot}ha^{-1}$로 나타났으며, 연간 탄소흡수량은 각각 7.99, $17.41ton{\cdot}ha^{-1}{\cdot}yr^{-1}$로 나타났다. 사문암 지역은 연간 $5.3tonC{\cdot}ha^{-1}$, 비사문암 지역은 연간 $14.49tonC{\cdot}ha^{-1}$를 흡수하는 것으로 나타났다.

• The Korean Journal of Ecology
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• 제20권5호
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• pp.385-391
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• 1997

충남 광천과 홍성 일대의 사문암과 변성암 지역의 암석, 토양 및 출현빈도가 높은 대나물의 중금속 함량을 측정하여 사문암 토양의 독성화 정도와 식물체의 흡수관계를 조사하였다. Ni, Cr 및 Co는 사문암에 매우 높았으며 Zn, Sc, Mo 및 Fe 는 변성암에서 더 높았다. 사문암 풍화토에서는 Ni, Cr 및 Co가 높았으며 Zn과 Fe는 비사문암 풍화토(사문암 및 변성암 풍화토와 변성암 풍화토)에서 높았고, 토양의 중금속은 암석내의 함량보다 낮았다. 사문암 풍화토에 출현하는 대나물내 중금속 함량은 혼합 풍화토의 그것보다 높게 나타났으며, 같은 사문암 지역이라도 홍성보다 광천의 중금속 함량이 높았다. 대나물의 평균 Fe:Ni의 비율은 혼합 풍화토에서는 216이고 사문암 풍화토에서는 49였다. 대나물내 Ni, Cr, Co, Fe 및 Sc 등은 지상부보다 지하부에서 높았으며, Zn과 Mo 함량은 지상부에서 높았다. 암석과 식물체의 중금속 함량 비교 결과 식물체에서보다 암석의 중금속 함량이 높았고, 대나물에 의한 Zn의 흡수는 사문암과 변성암 지역에서 높았으며 Sc와 Fe는 사문암 지역에서 뚜렷이 높았다.

• 한국환경생태학회지
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• 제12권1호
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• pp.22-29
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• 1998

충남지역의 사문암과 변성암 및 흑색셰일지역의 암석, 토양 및 그 위에서 생육하는 리기다소나무의 미량원소 함량을 측정하여 모암별 토양의 원소함량과 식물체의 흡수확계를 조사하였다. Ni, Cr 및 Co 함량은 사문암에서 매우 높았으며, Zn, Mo 및 Fe 함량은 변성암에서 높았다. 흑색셰일의 이들 원소는 사문암과 변성암보다 공히 낮았다. 사문암 토양의 Ni, Cr 및 Co 함량은 매우 높았으며, Zn과 Fe 함량은 사문암+변성암 혼합풍화토 및 흑색셰일 토양에서 높았다. 풍화토의 미량원소 함량은 암석의 함량보다 낮았으며, 그 패턴은 Mo를 제외하고는 모두 유사하였다. 사문암 풍화토의 pH 범위는 7.73~9.55로 매우 높았다. 사문암지역 리기다소나무의 Cr 흡수량은 토양내 Cr함량에 비하여 낮았으며, Zn 은 토양내의 원소함량에 비하여 리기다소나무에 의한 흡수량이 높았다. 리기다소나무에 의하여 흡수된 Ni, Fe 및 Co 함량에 대한 Fe/Ni, Co/Ni 비율은 사문암풍화토에서 가장 낮았다.

• 한국환경과학회지
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• 제18권6호
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• pp.621-632
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• 2009

Rare earth contents(REE) were analysed for the plants, M. sinensis. A. vulgaris and R. crataegitolius, from two different soils serpentine area consisting of serpentinite(SP) and non-serpentine area, containing amphibole schist(AS) of Gapyeong area, and were compared with soils and host rocks. The AS were high with the differences of several times in the top soils, and with the differences of several to ten times in the host rocks relative to the SP. In the same area, the SP were high in the soil, but the rocks for the AS. In the plants, the A. vulgaris were high, but low in the R. crataegitolius. Root parts were higher than the upper parts. Differences between the upper and root parts were big in the SP rather than the AS, and were big in the R. crataegitolius, but small in the M. sinensis. Among the parts of the plants, high elements were shown in the R. crataegitolius of the SP, and the A. vulgaris and M. sinensis of the AS. In the correlation coefficients, most of the REE showed positive relationships among the element pairs, especially high positive correlation coefficients in the upper parts of the SP.Differences of the soils and plants(average) were smalle in the M. sinensis and big in the R. crataegitolius. In the upper parts. contents of the A. vulgaris were close to the soils while the R. crataegitolius showed large discrepancies with the soils. In the root parts, contents of the A. vulgaris showed discrepancies with the soils regardless of soil types, but close in the R. crataegitolius of the SP and M. sinensis of the AS.

• 한국동물학회:학술대회논문집
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• 한국동물학회 1997년도 한국생물과학협회 학술발표대회
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• pp.164.1-164
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• 1997

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