Effects of Carrier on the Performance of a Methane Fermentation System Using Heat from a Hot Spring

Poster Sessio

Environmental Impacts of Methane Fermentation System Using Hot Springs

Penelitian ini bertujuan untuk mengetahui kompetensi pedagogik guru dalam proses pembelajaran PAI di MTs Pondok Pesantren Yayasan Hidayatul Ma’arifiyah Kecamatan Pangkalan Kerinci Kabupaten Pelalawan dan faktor faktor yang mempengaruhi kompetensi pedagogik guru dalam proses pembelajaran PAI di MTs Pondok Pesantren Yayasan Hidayatul Ma’arifiyah Kecamatan Pangkalan Kerinci Kabupaten Pelalawan. Subjek dalam penelitian ini adalah guru-guru PAI yang ada di MTs Pondok Pesantren Hidayatul Ma’arifiyyah Kecamatan Pangkalan Kerinci Kabupaten Pelalawan. Sedangkan yang menjadi objeknya adalah kompetensi pedagogik guru dalam proses pembelajaran PAI di MTs Pondok Pesantren Yayasan Hidayatul Ma’arifiyah Kecamatan Pangkalan Kerinci Kabupaten Pelalawan. Adapun teknik pengumpulan data yang digunakan yaitu observasi, wawancara, dan dokumentasi. Sedangkan teknik analisa data yang digunakan yaitu teknik deskriptif kualitatif dengan persentase. Berdasarkan hasil penelitian yang telah dilakukan maka penulis dapat mengambil kesimpulan yaitu: Kompetensi pedagogik guru dalam proses pembelajaran Pendidikan Agama Islam di MTs Hidayatul Ma’arifiyah Pangkalan Kerinci termasuk kategori cukup. Hal ini diketahui dari hasil persentase rata-rata kompetensi pedagogik guru dalam proses pembelajaran Pendidikan Agama Islam di MTs Hidayatul Ma’arifiyah Pangkalan Kerinci yaitu sebesar 60,67%. Sedangkan faktor-faktor yang mempengaruhi kompetensi pedagogik guru dalam proses pembelajaran PAI di MTs Hidayatul Ma’arifiyah Kecamatan Pangkalan Kerinci yaitu: latar belakang pendidikan guru, pengalaman mengajar, pengawasan yang dilakukan oleh kepada sekolah, dan sarana atau fasilitas pendidikan yang memadai yang dimiliki oleh MTs Hidayatul Ma’arifiyah Pangkalan Kerinci Kabupaten Pelalawan tersebut

A simple method for studying the molecular mechanisms of ultraviolet and violet reception in vertebrates

The Νmaxs and A/B ratios of HBNs of ancestral and present-day pigments. (DOCX 43 kb

Water transport model during CAPD: Determination of parameters

Water transport model during CAPD: Determination of parameters. To minimize the total amount of glucose required for removing the same volume of water as a bolus, a continuous infusion of glucose during CAPD was proposed and studied. Both a computer simulation of water transport through the peritoneal membrane and in vivo assessment with rats were carried out to evaluate the feasibility of the newly proposed mathematical model in which lymphatic drainage of dialysate from the peritoneal cavity to lymphatic system was considered in addition to conventional water transport. Mass transport area coefficients (KA) of 0.041 to 0.063 ml/min/100 g body wt and 0.045 to 0.066 ml/min/100 g body wt were measured for glucose and urea during CAPD with male Wistar rats. Hydraulic conductivity of peritoneal membrane (Lc) was 7.9 × 10-5 to 1.5 × 10-4 ml/min/mm Hg/100 g body wt, which was calculated by a linear relationship between volume and osmotic pressure. Simulated water transport model using determined parameters indicated that the ratio of lymphatic transport to convective transport would be changeable in CAPD with glucose infusion at varying infusion rates, while up to 16% of the glucose uptake could be reduced compared with that of the common CAPD at the same dwell time

Reconnaissance on Liquefaction-induced Flow Failure Caused by the 2018 Mw 7.5 Sulawesi Earthquake, Palu, Indonesia

The Mw 7.5 Sulawesi Earthquake 2018 was a catastrophic disaster that resulted in large numbers of casualties. This study aimed to investigate the damages of liquefaction-induced-flow failure in three areas in Palu city, i.e. Petobo, Balaroa, and Jono Oge. It was found that this flow failure occurred on a large scale at a very gentle ground inclination, ranging from 1 to 3%. In order to gain an understanding of the soil conditions in these specific locations, Portable Dynamic Cone Penetration Tests were conducted in Petobo. The results showed that the soil layers in the affected area were in a loose state compared to the non-affected areas. Furthermore, some spots of freshwater inundation were recognized in Petobo and Balaroa, even two weeks after the disaster. Based on this evidence, a mechanism of liquefaction-induced-flow failure caused by a confined aquifer is proposed