The research about seismik microzonation using HVSR methods in Lili village, sub-district of Fatuleu, district of Kupang has been done. The aims of this research are to determine the values of soil dominant frequency, magnitude of amplification, seismik vulnerability index, and the peak ground acceleration. This research used TDS 303S type with0,2Hz-20Hz of natural frequency. According to this research, it was obtained that the values of the dominant frequency was about 0,279Hz-17,210Hz, the amplification values were found to be 1,802-10,240 and the index of vulnerability has values about 0,422-421,167. The peak ground acceleration values about 160,769 gal – 279,316 gal with great risk level two and great risk level three.

We made maps of areas prone to erosion in Timor Tengah Selatan regency, province of East Nusa Tenggara using remote sensing and geographic information system. The purpose of this study is to map areas prone to erosion and risks assessment in Timor Tengah Selatan regency East Nusa Tenggara province .The research methods include the use of GIS to make rainfall, land cover map and class slopes map. Based on the results, level of erosion can be divided into three classes. First, areas which are not prone to erosion (127.218,69 Ha), covering districts Noebeba, districts Amanuban South, districts Kualin, most districts Amanuban East and districts Fatukopa. Second, areas prone to erosion (251.082.09 Ha) covering almost all districts Timor Tengah Selatan. Third, areas highly prone to erosion (9.125,1 Ha) covering an area districts Fatumasi, districts Tobu, Mollo Utara, districts, most districts Kot`olin.

The research about seismic microzonation in Nunkurus village, sub-district of east Kupang, district of Kupang has been done. The aims of this research are to determine the values of soil dominant frequency, magnitude of amplification, seismic vulnerability index, the peak ground acceleration and to make seismic vulnerability index map and PGA map. The results showed that the values of the the values of the dominant frequency was about 0,293 Hz – 18,41 Hz, the amplification about 1,68 – 8,52. Meanwhile, the index of vulnerability was found to be 0,32853 – 179,23556 and peak ground acceleration values about 107,77488 gal - 218,62941 gal so it can be said that the area of ??research is safe enough because only a single point that has the frequency value, the value of amplification, the index value of vulnerability and PGA great value.

A research has been done with used geomagnetic method in located science centre of oelnasi village subdistric kupang centre, kupang regency. This research purposes for interpretation under surface condition site the building of science centre and mapped pattern rock layered under surface in the location research. Acquire data to do in 192 drop measure with wide located ± 50 hectare. The acquire process with looping system make use of Proton Prosession Magnetometer (PPM) type GSM-19T. Output research showed value spread total intensity magnetic field as of 45255,85 nT to 45517,70 nT. For output anomaly data processing get to turn -90 nT to 190 nT. Two dimantion output modeling showed that in the location research predominance of limestones rock with the susceptibility value 0,000002 cgs unit to 0,002778 cgs unit and be in the depth ±0 meters – 20 meters, and diamagnetic rock with the susceptibility value -0,000013 cgs unit to 0,000840 cgs unit be in the depth ±5 meters – 20 meters.

Variasi perubahan frekuensi kritis lapisan F2 (foF2) dan ketinggian lapisan F2 (hF2) di atas Kupang selama tahun 2014 mengalami perubahan yang bervariasi dimana hal ini bergantung pada aktivitas matahari, semakin tinggi tingkat aktivitas matahari semakin tinggi pula tingkat variasi pada foF2 dan hF2, sebaliknya semakin rendah tingkat aktivitas matahari semakin berkurang pula tingkat variasi foF2 dan hF2 variasi perubahan terhadap lapisan F diindikasikan dengan penurunan dan peningkatan nilai foF2 dan hF2. Peningkatan nilai foF2 rata-rata terjadi pada pukul 07.00 WITA mencapai maksimumnya pada pukul 12.00-14.00 WITA siang hari dan dikuti dengan penurunan nilai foF2 pada malam hari yang mencapai minimumnya pada pukul 05.00-06.00 WITA pagi. Selama tahun 2014, ketinggian lapisan F2 memiliki tiga pola peningkatan yang berbeda, (1) peningkatan ketinggian pada jam tengah hari seperti yang terjadi pada bulan Januari – April, (2) peningkatan pada jam tengah malam hingga menjelang matahari terbit, jam-jam tengah hari dan sore hingga malam hari terjadi pada bulan Mei – Agustus (3) peningkatan pada pada jam tengah malam hingga menjelang matahari terbit dan jam-jam tengah hari seperti pada bulan September – Desember. Dalam pemanfaatannya sebagai media pantul gelombang komunikasi radio frekuensi tinggi (HF), karakteristik ionosfer di atas Kupang selama tahun 2014, memiliki kemampuan memantulkan gelombang frekuensi tinggi berada pada rentang 2-19.2 MHz dengan ketinggian yang berada pada rentang 179 – 550 Km. Akan mengakibatkan gagalnya komunikasi radio frekuensi tinggi, apabila menggunakan frekuensi lebih besar atau lebih kecil dari frekuensi yang dapat bekerja tersebut.

A monocular light microscope with three objective lenses of size 4X, 10X, and 40X and two types of 10X and 16X ocular lenses has been updated into a digital microscope using a digital camera with a resolution of 1600 x 1200 pixel. The update of light microscope is also used as for high school students learning, so that the results of observations can be interpreted quantitatively. The digital microscopes, has been equipped with a computer system using LattePanda computer boards and features a 10.1 inch touch screen to facilitate the user of this microscope in making observations. To be able to use this microscope, a software has been designed using Delphi 10 which can view and store the results of observations quantitatively.

A research of bricks from clay withouth mixture of rice husks from Tanah Merah Village-Kupang District-East Nusa Tenggara with temperature of 800oC, 900oC, and 1000oC has been done. The aim of this research is to determine quality of bricks from clay. Based on the result of this research, brick with temperature of 800oC has density value 1,12 gram/cm3, brick with temperature of 900oC has density value 1,002 gram/cm3, and brick with temperature of 1000oC has density value 1,15 gram/cm3. Compressive strength at temperature of 800oC is 2,73 N/mm2, compressive strength at temperature of 900oC is 1,38 N/mm2 and at the temperature of 1000oC is 4,09 N/mm2. For water absorption in the third temperature treatment are 1,39% 2,82% dan 1,42%. Grain size at temperature of 800oC has the smallest size is 28,5 x 10-6 meter and the largest size is 85,7 x 10-5 meter, grain size at temperature of 900oC has the smallest size is 57,1 x 10-6 meters and the largest size is 1,28571 x 10-3 meters, grain size at temperature of 1000oC has smallest size is 30 x 10-6 meters and the largest size is 67,5 x 10-5 meters.