<?xml version="1.0" encoding="UTF-8" ?>
<modsCollection xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://www.loc.gov/mods/v3" xmlns:slims="http://slims.web.id" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-3.xsd">
<mods version="3.3" id="1706315">
 <titleInfo>
  <title>KAJIAN DISTRIBUSI ALIRAN INTAKE KE PLTMH AKIBAT PERUBAHAN  ALIRAN DI HULU SUNGAI</title>
 </titleInfo>
 <name type="Personal Name" authority="">
  <namePart>SUFRIZALIANSYAH</namePart>
  <role>
   <roleTerm type="text">Primary Author</roleTerm>
  </role>
 </name>
 <typeOfResource manuscript="no" collection="yes">mixed material</typeOfResource>
 <genre authority="marcgt">bibliography</genre>
 <originInfo>
  <place>
   <placeTerm type="text">Banda Aceh</placeTerm>
   <publisher>PROG. STUDI MAGISTER TEKNIK MESIN</publisher>
   <dateIssued>2013</dateIssued>
  </place>
 </originInfo>
 <language>
  <languageTerm type="code">id</languageTerm>
  <languageTerm type="text">Indonesia</languageTerm>
 </language>
 <physicalDescription>
  <form authority="gmd">Theses</form>
  <extent></extent>
 </physicalDescription>
 <note>Micro  hydro  Power (MHP)  Rampah  planned  to  power  as many  as 95 heads  of house  holds with an installed  power  capacity of 20 kW. Source  water comes  from rivers  by building  dams Rampah  intake.  Intake  should  be on the  basis  of a steady  stream,  so  it does  not  impede  the flow of water entering the intake.  The writing  is focused on the stability  of the river going  up stream  along  the  300  m   intake,  based  on  the  difference  between the  two  cross-sectional sediment capacity in  each  pias.  Stream  flow  that  occurred during  measurements of 5.724 m'/sec. Debit is used to drive a 50%  of the measured discharge, so the  available flow is 2.862 m'/sec. This  exceeds   the  initial  survey  of potential discharge   stream Rampah  required to drive  the  turbine   at  MHP  Rampah  of  1.5   m'/sec.  Calculation of  sediment using   Frylink method. Turns  on  up  stream  erosion,  so that  down  stream  erosion,   while  experiencing the process  of deposition of sediment down  stream.  Debit  dominant flooding  that  occurred   in September  2011  until   February   2012 amounted  to  9.833  m'/sec  and  a  maximum   flood discharge of  19.572 m/sec. While  the  discharge monitoring using  arc  discharge  regression equation         Q = (3.142 H -0.289. In the circumstances the magnitude of dominant flood sediments  (bed  load)  that  settles  and  into  the  intake  tract  of 0.00019 m/sec, while  in a state of maximum  flood  0.00035  m'  /sec.  Minimum  grain  diameter (smallest)  as the  protector of the river at flood dominant at 21.50 mm, and maximum  flood conditions used by 31.00 mm.&#13;
&#13;
Keywords  : Debit,  sedimentation, stability.&#13;
</note>
 <note type="statement of responsibility"></note>
 <subject authority="">
  <topic>ELECTRIC GENERATORS</topic>
 </subject>
 <classification>621.313</classification>
 <identifier type="isbn"></identifier>
 <location>
  <physicalLocation>ELECTRONIC THESES AND DISSERTATION Universitas Syiah Kuala</physicalLocation>
  <shelfLocator></shelfLocator>
 </location>
 <slims:digitals/>
</mods>
<recordInfo>
 <recordIdentifier>1706315</recordIdentifier>
 <recordCreationDate encoding="w3cdtf">2025-11-06 15:47:36</recordCreationDate>
 <recordChangeDate encoding="w3cdtf">2025-11-07 10:14:46</recordChangeDate>
 <recordOrigin>machine generated</recordOrigin>
</recordInfo>
</modsCollection>