본 연구에서는 입계의 성질을 이용한 PTCR 재료에 입계 modifier로서 Bi2O3를 첨가하고 입계의 미세구조와 결함농도를 변화시켜 이에 따른 소결 및 전기적 특성변화를 TMA, XRD, 복합 임피던스방법 등을 이용하여 해석하였다. 실험 결과 Y이 도우핑된 BaTiO3PTCR 재료에 Bi2O3를 첨가하였을때 약 0.1mol%까지 고용이 되는 것으로 밝혀졌다. Bi2O3를 고용한계 이하로 첨가시에는 생성되는 vacancy등의 결함으로 말미암아 Y-BaTiO3의 치밀화가 촉진되었으나, 그 이상 첨가하면 치밀화 뿐만 아니라 결정립 성장도 억제되었다. Bi2O3의 첨가량에 따라 계내에 존재하는 각 이온의 반경, 결함 반응식 및 격자 탄성 변형 에너지 등을 고려하면 Y-BaTiO3결정립 내부에 Ba와 Ti vacancy가 동시에 생길 수 있어 고온저항이 높아짐을 알 수 있었다. BN은 BaTiO3에 고용이 되지 않는 것으로 밝혀졌으며 B2O3를 주성분으로한 액상형성으로 인하여 저온에서의 급격한 치밀화가 관찰되었다. 또 Ba-Y-Ti-B-O의 비정질 상이 tripie junction에 존재함으로써 상온저항이 크게 변화하였으며, PTCR jump도 높아졌다.

Gastrointestinal stromal tumor (GIST) is the most common soft tissue sarcoma of the gastrointestinal tract. Surgery is the primary treatment of choice for patients with localized or potentially resectable GIST, whereas imatinib is the main treatment for patients with advanced, unresectable, or metastatic GIST. Neoadjuvant treatment with imatinib is not routinely recommended unless there is significant justification for reducing the tumor size in order to improve surgical outcome. The authors describe a case of a 48-year-old man who confirmed huge rectal GIST, and received successful neoadjuvant treatment with imatinib for preserving anal sphincter function followed by transanal excision.

Abnormal change in Gyeongpo beach shoreline in June of 2012 was illustrated using DGPS (Differential Global Positioning System, resolution < 0.6m) observation and drift experiment. Abrupt change in the shoreline was occurred in the latter part of June, 2012, this change was compared with that in June from 2009 to 2011. In the northern part of the beach, sand accumulated and it made beach extension and movement of the shoreline towards sea compared with that in June from 2009 to 2011. While on the other, in the southern part, the beach was eroded and it formed a steep slope around the southernmost of the beach. The shoreline in the southern part of the beach was shifted more towards land than that in the past. Change in the position of shoreline was higher in the northernmost and southernmost of the beach compared with those in the other parts. Drift in the southern part of the beach moved faster along the beach than that in the northern part of it.