Perubahan Tingkat Kecemasan Pasien Pre Operasi dengan Terapi Murottal Al-Qur'an di RSUD Raden Mattaher Jambi

Pasien yang akan menjalani operasi, peningkatan tekanan darah dan nadi sering kali terjadi, salah satu penyebabnya adalah kecemasan yang menyebabkan penundaan operasi yang akan dijalani. Data WHO pada tahun 2013 mengemukakan bahwa jumlah pasien yang melakukan operasi mencapai angka 148 juta jiwa. Salah satu teknik distraksi keagamaan adalah terapi murottal Al-Qur'an. Penelitian ini bertujuan untuk mengetahui pengaruh terapi murottal al-qur'an terhadap Perubahan tingkat kecemasan pasien pre operasi di RSUD Raden Mattaher Jambi. Penelitian ini merupakan penelitian kuantitatif dengan metode pra eksperimen dengan rancangan pretest posttest one grup design without control. Populasinya yaitu pasien yang menjalani operasi sebanyak 2902 pasien. Pengambilan sampel dilakukan dengan menggunakan teknik accidental sampling yaitu berjumlah 14 pasien pre operasi. Instrumen penelitian yaitu Amsterdam Preoperatif Anxiety and Information Scale (APAIS). Analisa data dalam penelitian ini secara univariat dan bivariat dengan menggunakan Uji Wilcoxon. Hasil analisis menunjukkan bahwa ada Perubahan tingkat kecemasan pasien pre operasi dengan terapi terapi murottal Al-Qur'an dengan p-value 0,01 pada pasien pre operasi di RSUD raden Mattaher Jambi. Diharapkan penelitian ini dapat menjadi masukan dan informasi bagi pihak rumah sakit tentang pengaruh pemberian terapi murottal al-qur'an terhadap Perubahan tingkat kecemasan pasien pre operasi agar dapat dilakukan pemberian terapi murottal al-qur'an dalam penanganan kecemasan

Pengaruh Metode Pengeringan Terhadap Kualitas Simplisia Lempuyang Wangi (Zingiber Aromaticum L.)

Pengeringan merupakan tahapan terpenting dalam menjaga kestabilan senyawa pada simplisia. Simplisia tanaman lempuyang wangi sejak lama dikenal sebagai bahan ramuan obat untuk diare, disentri penyakit kulit dan antimikroba. dikenal sebagai bahan ramuan obat untuk diare, disentri penyakit kulit dan antimikroba. Penelitian ini dilaksanakan di Balai Besar Penelitian dan Pengembangan Tanaman dan Obat (B2P2TO2T). Penelitian ini bertujuan untuk mengetahui pengaruh metode pengeringan terhadap biomasa, kadar air, rendemen minyak atsiri dan nilai kesukaan terhadap simplisia tanaman lempuyang wangi. Metode pengeringan yang digunakan adalah pengeringan dengan oven 50oC, pengeringan sinar matahari langsung dan kering angin. Parameter yang diamati yaitu biomasa, kadar air, rendemen minyak atsiri dan nilai kesukaan. Hasilnya menunjukkan pengeringan menggunakan oven suhu 50oC merupakan pengeringan yang paling baik dengan kadar air paling sedikit 8.4%, rendemen minyak atsiri paling banyak 0.87 % meskipun biomasa paling sedikit yakni 239,36 g

Continent formation through time

The continental crust is the primary archive of geological history, and is host to most of our natural resources. Thus, the following remain critical questions in Earth Science, and provide an underlying theme to all of the contributions within this volume: when, how and where did the continental crust form? How did it differentiate and evolve through time? How has it has been preserved in the geological record? This introductory review provides a background to these themes, and provides an outline of the contributions contained within this volum

Pengaruh Pupuk Organik Cair Berbahan Dasar Limbah Sawi Putih (Brassica Chinensis L.) Terhadap Pertumbuhan Tanaman Jagung Manis

Liquid organic fertilizer was a fertilizer that comes from nature and served to increase the physical, chemical and biological condition of soil. It contains nutrient that be able to improve plants growth. The purpose of this experiment was to observe the effect of liquid organic fertilizer from waste of China cabbage on the growth of sweet corn. The research was conducted in Laboratory of Biology, Diponegoro University. The research design used was a completely randomized design witha single factor, namely the concentration of liquid organic fertilizer in 6 treatments and 5 replication that. The treatments were control (without fertilizer), 1 mL/L, 2 mL/L, 3 mL/L, 4 mL/L, 5 mL/L. The data were analyzed by Analysis of Variance (ANOVA) at 95% significance level. Parameters observed were plant height, number of leaves, fresh weight and dry weight. The results showed that treatment of liquid organic fertilizer spraying with different concentrations affect on all growth parameters. Concentration of 3 mL/L produced the highest plant, the concentration of 1 mL/Land 4 mL/L resulted in the highest number of leaves. The highest of fresh and dry weight were resulted by application of 1 mL/L liquid organic fertilizer

Cascade Boltzmann - Langevin approach to higher-order current correlations in diffusive metal contacts

The Boltzmann - Langevin approach is extended to calculations of third and fourth cumulants of current in diffusive-metal contacts. These cumulants result from indirect correlations between current fluctuations, which may be considered as "noise of noise". The calculated third cumulant coincides exactly with its quantum-mechanical value. The fourth cumulant tends to its quantum-mechanical value $-e^3I/105$ at high voltages and to a positive value $2e^2T/3R$ at V=0 changing its sign at $eV \sim 20T$.Comment: 6 pages, 2 eps figures, typo corrected, minor change

Effect of deformation on components of internal stress tensor in grains of FCC-polycristal

Study of contributions of internal stress tensor components in deformed of austenitic steel was carriedout. The tensor components of internal stresses were determined with using bending extinction contours observing on electron microscope images of the steel

Triple oxygen isotopic composition of the high-³He/⁴He mantle

Measurements of Xe isotope ratios in ocean island basalts (OIB) suggest that Earth’s mantle accreted heterogeneously, and that compositional remnants of accretion are sampled by modern, high-3He/4He OIB associated with the Icelandic and Samoan plumes. If so, the high-3He/4He source may also have a distinct oxygen isotopic composition from the rest of the mantle. Here, we test if the major elements of the high-3He/4He source preserve any evidence of heterogeneous accretion using measurements of three oxygen isotopes on olivine from a variety of high-3He/4He OIB locations. To high precision, the Δ17O value of high-3He/4He olivines from Hawaii, Pitcairn, Baffin Island and Samoa, are indistinguishable from bulk mantle olivine (Δ17OBulk Mantle − Δ17OHigh 3He/4He olivine = −0.002 ± 0.004 (2 × SEM)‰). Thus, there is no resolvable oxygen isotope evidence for heterogeneous accretion in the high-3He/4He source. Modelling of mixing processes indicates that if an early-forming, oxygen-isotope distinct mantle did exist, either the anomaly was extremely small, or the anomaly was homogenised away by later mantle convection. The δ18O values of olivine with the highest 3He/4He ratios from a variety of OIB locations have a relatively uniform composition (∼5‰). This composition is intermediate to values associated with the depleted MORB mantle and the average mantle. Similarly, δ18O values of olivine from high-3He/4He OIB correlate with radiogenic isotope ratios of He, Sr, and Nd. Combined, this suggests that magmatic oxygen is sourced from the same mantle as other, more incompatible elements and that the intermediate δ18O value is a feature of the high-3He/4He mantle source. The processes responsible for the δ18O signature of high-3He/4He mantle are not certain, but δ18O–87Sr/86Sr correlations indicate that it may be connected to a predominance of a HIMU-like (high U/Pb) component or other moderate δ18O components recycled into the high-3He/4He source

Nickel and helium evidence for melt above the core–mantle boundary

High ^(3)He/^(4)He ratios in some basalts have generally been interpreted as originating in an incompletely degassed lower-mantle source. This helium source may have been isolated at the core–mantle boundary region since Earth’s accretion. Alternatively, it may have taken part in whole-mantle convection and crust production over the age of the Earth; if so, it is now either a primitive refugium at the core–mantle boundary or is distributed throughout the lower mantle. Here we constrain the problem using lavas from Baffin Island, West Greenland, the Ontong Java Plateau, Isla Gorgona and Fernandina (Galapagos). Olivine phenocryst compositions show that these lavas originated from a peridotite source that was about 20 per cent higher in nickel content than in the modern mid-ocean-ridge basalt source. Where data are available, these lavas also have high ^(3)He/^(4)He. We propose that a less-degassed nickel-rich source formed by core–mantle interaction during the crystallization of a melt-rich layer or basal magma ocean, and that this source continues to be sampled by mantle plumes. The spatial distribution of this source may be constrained by nickel partitioning experiments at the pressures of the core–mantle boundary

A murine model of Charcot-Marie-Tooth disease 4F reveals a role for the C-terminus of periaxin in the formation and stabilization of Cajal bands

Charcot-Marie-Tooth (CMT) disease comprises up to 80 monogenic inherited neuropathies of the peripheral nervous system (PNS) that collectively result in demyelination and axon degeneration. The majority of CMT disease is primarily either dysmyelinating or demyelinating in which mutations affect the ability of Schwann cells to either assemble or stabilize peripheral nerve myelin. CMT4F is a recessive demyelinating form of the disease caused by mutations in the Periaxin (PRX) gene. Periaxin (Prx) interacts with Dystrophin Related Protein 2 (Drp2) in an adhesion complex with the laminin receptor Dystroglycan (Dag). In mice the Prx/Drp2/Dag complex assembles adhesive domains at the interface between the abaxonal surface of the myelin sheath and the cytoplasmic surface of the Schwann cell plasma membrane. Assembly of these appositions causes the formation of cytoplasmic channels called Cajal bands beneath the surface of the Schwann cell plasma membrane. Loss of either Periaxin or Drp2 disrupts the appositions and causes CMT in both mouse and man. In a mouse model of CMT4F, complete loss of Periaxin first prevents normal Schwann cell elongation resulting in abnormally short internodal distances which can reduce nerve conduction velocity, and subsequently precipitates demyelination. Distinct functional domains responsible for Periaxin homodimerization and interaction with Drp2 to form the Prx/Drp2/Dag complex have been identified at the N-terminus of Periaxin. However, CMT4F can also be caused by a mutation that results in the truncation of Periaxin at the extreme C-terminus with the loss of 391 amino acids. By modelling this in mice, we show that loss of the C-terminus of Periaxin results in a surprising reduction in Drp2. This would be predicted to cause the observed instability of both appositions and myelin, and contribute significantly to the clinical phenotype in CMT4F

Boron isotopic composition of olivine-hosted melt inclusions from Gorgona komatiites, Colombia : new evidence supporting wet komatiite origin

Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Earth and Planetary Science Letters 312 (2011): 201–212, doi:10.1016/j.epsl.2011.09.033.A fundamental question in the genesis of komatiites is whether 30 these rocks originate from partial melting of dry and hot mantle, 400−500°C hotter than typical sources of MORB and OIB magmas, or if they were produced by hydrous melting of the source at much lower temperatures, similar or only moderately higher than those known today. Gorgona Island, Colombia, is a unique place where Phanerozoic komatiites occur and whose origin is directly connected to the formation of the Caribbean Large Igneous Province. The genesis of Gorgona komatiites remains controversial, mostly because of the uncertain origin of volatile components which they appear to contain. These volatiles could equally result from shallow level magma contamination, melting of a “damp” mantle or fluid-induced partial melting of the source due to devolatilization of the ancient subducting plate. We have analyzed boron isotopes of olivine40 hosted melt inclusions from the Gorgona komatiites. These inclusions are characterized by relatively high contents of volatile components and boron (0.2−1.0 wt.% H2O, 0.05−0.08 wt.% S, 0.02−0.03 wt.% Cl, 0.6−2.0 μg/g B), displaying positive anomalies in the overall depleted, primitive mantle (PM) normalized trace element and REE spectra ([La/Sm]n = 0.16−0.35; [H2O/Nb]n = 8−44; [Cl/Nb]n = 27−68; [B/Nb]n = 9-30, assuming 300 μg/g H2O, 8 μg/g Cl and 0.1 μg/g B in PM; Kamenetsky et al., 2010. Composition and temperature of komatiite melts from Gorgona Island constrained from olivine-hosted melt inclusions. Geology 38, 1003–1006). The inclusions range in δ11B values from −11.5 to +15.6 ± 2.2‰ (1 SE), forming two distinct trends in a δ11B vs. B-concentration diagram. Direct assimilation of seawater, seawater-derived components, altered oceanic crust or marine sediments by ascending komatiite magma cannot readily account for the volatile contents and B isotope variations. Alternatively, injection of <3% of a 11B enriched fluid to the mantle source could be a plausible explanation for the δ11B range that also may explain the H2O, Cl and B excess.Financial support to AAG during data acquisition and manuscript preparation was provided by Northeast National Ion Microprobe Facility (Woods Hole Oceanographic Institution, USA) and the Centre de Recherches Pétrographiqueset Géochimiques (France). This research was also supported by the Australian Research Council (Research Fellowship and Discovery grants to VSK). We acknowledge partial support of the Alexander von Humboldt Foundation, Germany (F.W. Bessel Award to VSK and Wolfgang Paul Award to A.V. Sobolev who provided access to the electron microprobe at the Max Planck Institute, Mainz, Germany