본 연구는 산마늘의 임간재배를 위한 기초 환경자료를 제공하고자 실시하였다. 울릉도 산마늘은 너도밤나무, 우산고로쇠나무, 섬잣나무, 솔송나무, 소나무, 곰솔, 섬피나무, 두메오리나무 군락에 자생하고 있으며, 입지환경은 평균 해발고도 563.4 m, 평균 경사는 27.8°이었다. 토성은 사토, 사질양토, 양질사토, 양토가 다양하게 나타났으며, 유기물층의 깊이는 평균 6 cm, 토양 pH는 5.40, 유효인산은 18.5 ppm, 양이온 치환용량은 18.6 cmolc/kg으로 나타났다. CCA분석에 의한 입지와 토양인자와의 상관관계를 보면 너도밤나무군락은 탄소, 질소, 모래함량, 양이온치환용량과 정의 상관관계를 나타내었다.

실험실에서 형질전환될 수 있는 세균들은 자연환경 조건에서도 형질전환 능력이 발달하는 것으로 알려져 있다. 따라서, 환경 내에서 형질전환 능력이 있는 세균의 존재는 확실한 것으로 여겨진다. DNA는 무기물에 부착된 상태에서는 핵산분해효소에 의한 분해로부터 보호되는 것으로 알려져 있다. 비록 DNA가 토양 속에 분산되어져 일정 비율로 가수분해되더라도, 수 주일 후에도 낮은 비율로 감지될 수 있다. 따라서 free DNA는 자연적 형질전환을 할 수 있을 만큼

Development of appropriate construction technology at frozen soil environments for developing resources is essential. However, cathodic protection technology using monitoring at frozen soil environments is lack. In this study, we want to build a real-time monitoring system at frozen soil environments through corrosion monitoring using type of gavanic metal

Extensive land subsidence and submergence occurred in the coal mining areas (Huainan and Huaibei) in Anhui Province, China. As a result, lots of subsided lakes have been formed due to their unique geological features. Four typical lakes were selected to evaluate the internal phosphorus (P) releasing risk based on the specification of P, Fe and Al from the sediments. Sediment P, Fe and Al in the top 5 cm were extracted sequentially, aiming at obtained fractionation for environmental indicators. Experiments of P isothermal adsorption were conducted to characterize P sorption ability. The results suggested that P internal loading potential was related to Al and Fe compounds in sedimentary environments of soil inundation, primarily determined by regional soil properties. Internal P releasing risk was mainly controlled by the properties of calcareous soils in the Huaibei; whereas controlled by Fe and Al in the Huainan. Overall, the obtained results fit well with the model proposed by Kopáček et al.(2005), which predicted low P flux as molar ratio of [NH4Cl-Al + BD-Al + NaOH-Al] : [NH4Cl-Fe + BD-Fe] >3 or [NaOH-Al] : [NH4Cl-P + BD-P] >25 from sediments when anoxia is developed. However, this threshold has site-specific flexibility, with its lower limit approaching 20:1 applicable for the three lakes in Huainan. Higher loads of external input organic matters or enriched Fe oxides bound P tend to change this limit and lead to internal loading risk with environmental anoxia.