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M. Noor
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Agriculture, Biological Sciences & Forestry Health Professions Medicine & Pharmacology

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Faktor-Faktor yang Mempengaruhi Kejadian Pneumonia pada Balita di Wilayah Kerja Puskesmas Guntung Payung Tahun 2013 M. Noor; Sugeng Riyanto; Mutiara Kusuma Wardani; STIKES Husada Borneo; Alumni STIKES Husada Borneo
Jurnal Kesehatan Indonesia Vol 4 No 2 (2014): Maret
Publisher : HB PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (136.895 KB)

Abstract

Pneunomia is infection in lower respiratory tract and it is a health problem in the world because of its high number of death, predicted more than 2 million of children under five years death because of pneumonia compared to other diseases. Pneumonia on baby and children under five years caused by bacteria and virus andinfluenced by some factors, such as environmental factor,child individual factor and behavioral factor. Environmental factors consist of house condition covers density of the house, ventilation, humidity, lighting, and air pollution in the house. For child individual factors cover child age, birth weight, nutritional status, immunization status, and giving vitamin A. Behavioral factors cover parents’ knowledge, immediate action to disease and coverage of health services. This study aimed to know the factors which influenced pneumonia occurrence on children under five at working area of Guntung Payung Health Center of Banjarbaru in 2013. This study used analytic survey method with cross-sectional approach. Population in this study was all children under five in working area of Guntung Payung Health Center of Banjarbaru in 2013 with 92 respondents. Based on the result of chi-square test showed there was no correlation among, age, birth weight and giving vitamin A with pneumonia occurrence on children under five age. Whereas, there was correlation between immunization status of children under five and pneumonia occurrence at Guntung Payung Health Center of Banjarbaru in 2013.
The Effects of Drying and Wetting on the Soil Chemical Properties of Acid Sulphate Soils of Kalimantan M. NOOR; A. MAAS; T. NOTOHADIKUSUMO
Jurnal Tanah dan Iklim (Indonesian Soil and Climate Journal) No 27 (2008): Juli 2008
Publisher : Balai Besar Penelitian dan Pengembangan Sumberdaya Lahan Pertanian

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21082/jti.v0n27.2008.%p

Abstract

This research aimed to study the effects of land reclamation (drying, wetting, flushing, and leaching) on the change of soil chemical properties of acid sulphate soils from Kalimantan. Randomized Complete Design (RCD) by two factors treatments with two replications is used in this research. Factor I was soil reactiveness that is define as (a) low reactive= R1; (b)moderate reactive =R2; (c) strong reactive= R3, and (d) very strong reactive= R4 respectively. Factor II was drying, wetting, and diluting that is define as (1) drying continuously after wetting = W1, (2) wetting continuously = W2; (3) drying after weeting and diluting =W3; and (4) wetting and diluting. The result of experiments show that continuous drying after wetting (W1) and drying after wetting and diluting (W3) or continuous weeting (W2) gave soils pH lower than the weeting and diluting (W4).Dried on the strong reactive soils (R4) not decrease soil pH significantly. The continouos drying after wetting (W1) can increase EC (electrical conductivity) higher than the continous wetting (W2) and wetting that followed diluting (W4) or drying after wetting and diluting (W3). The continouos wetting (W2) and the continouos drying after wetting (W1) has given the total soluble acidity of 63,30 dan 61,71 cmolc kg-1 respectively, higher than drying after wetting and diluting (W3) and wetting thatfollowed diluting (W4) that given total soluble acidity of 54,03 and 51,95 cmolc kg-1 respectively. The effects of drying, wetting, flushing, and leaching on the total soluble acidity, Soluble Al and soluble H, especially on the strong reactive soils are very significant. All of the exchangeble bases (Ca, Mg, K, Na) on the continouos drying after wetting (W1) are lower than the continous wetting (W2) and wetting that followed diluting (W4)or drying after wetting and diluting (W3) respectively. The continouos drying after wetting (W1), the continous wetting (W2) and wetting that follow diluting (W4) or drying after wetting and diluting (W3) decrease exchangable Mg, especially on strong reactive soils (R4), but contradictive to low reactive soils (R1). The continouos drying after wetting (W1) increase exchangable Na, especially on low reactive soils (R1), but the wetting that followed diluting (W3, W4) decreases exchangable Na.
Co-Authors A. MAAS Alumni STIKES Husada Borneo Mutiara Kusuma Wardani STIKES Husada Borneo Sugeng Riyanto T. NOTOHADIKUSUMO