<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">BOUHADEB</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">BOUGUERRA H</style></author><author><style face="normal" font="default" size="100%">DERDOUS O</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessing soil loss using GIS based RUSLE methodology. Case of the Bou Namoussa watershed &amp;ndash; North-East of Algeria, 2018, PL ISSN 1429&amp;ndash;7426., Polish Academy of Sciences (PAN), Committee on Agronomic Sciences, Degruyte, DOI: 10.2478/jwld-2018</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Water and Land Development </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.itp.edu.pl/wydawnictwo/journal/36_2018_I_III/Bouhadeb.pdf</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 27–35</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:131.333px;top:688.416px;14.9711px;serif;transform:scaleX(1.00015);&quot;&gt;This study aims to estimating annual soil erosion rate and its &lt;/span&gt;&lt;span style=&quot;left:497.629px;top:688.416px;14.9711px;serif;transform:scaleX(1.00136);&quot;&gt;spatial distribution in the Bou Namoussa water-&lt;/span&gt;&lt;span style=&quot;left:105.963px;top:705.538px;14.9711px;serif;transform:scaleX(1.03121);&quot;&gt;shed located in the North-East of Algeria by applying the revis&lt;/span&gt;&lt;span style=&quot;left:493.416px;top:705.538px;14.9711px;serif;transform:scaleX(1.02336);&quot;&gt;ed universal soil loss equation (RUSLE) within &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:722.751px;14.9711px;serif;transform:scaleX(0.998512);&quot;&gt;a Geographical Information System environment (GIS). The applic&lt;/span&gt;&lt;span style=&quot;left:507.581px;top:722.751px;14.9711px;serif;transform:scaleX(0.999618);&quot;&gt;ation of the RUSLE model in different natural &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:739.963px;14.9711px;serif;transform:scaleX(1.00806);&quot;&gt;environments and on every scale takes into account five key fac&lt;/span&gt;&lt;span style=&quot;left:491.354px;top:739.963px;14.9711px;serif;transform:scaleX(1.01094);&quot;&gt;tors namely: the rainfall erosivity, the soil erodi-&lt;/span&gt;&lt;span style=&quot;left:105.963px;top:757.085px;14.9711px;serif;transform:scaleX(1.03489);&quot;&gt;bility, the steepness and length of slopes, the vegetation cove&lt;/span&gt;&lt;span style=&quot;left:482.837px;top:757.085px;14.9711px;serif;transform:scaleX(1.02999);&quot;&gt;r and the conservation support practices. Each of &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:774.298px;14.9711px;serif;transform:scaleX(1.01278);&quot;&gt;these factors was generated in GIS as a raster layer, their com&lt;/span&gt;&lt;span style=&quot;left:478.982px;top:774.298px;14.9711px;serif;transform:scaleX(1.01092);&quot;&gt;bination, resulted in the development of a soil loss &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:791.42px;14.9711px;serif;transform:scaleX(0.988245);&quot;&gt;map indicating an average erosion rate of 7.8 tꞏha&lt;/span&gt;&lt;span style=&quot;left:407.536px;top:789.41px;9.68188px;serif;transform:scaleX(1.00157);&quot;&gt;–1&lt;/span&gt;&lt;span style=&quot;left:417.217px;top:791.42px;14.9711px;serif;transform:scaleX(0.612241);&quot;&gt;ꞏy&lt;/span&gt;&lt;span style=&quot;left:429.678px;top:789.41px;9.68188px;serif;transform:scaleX(1.00157);&quot;&gt;–1&lt;/span&gt;&lt;span style=&quot;left:439.36px;top:791.42px;14.9711px;serif;transform:scaleX(1.01647);&quot;&gt;. The obtained soil loss map was classified into four ero-&lt;/span&gt;&lt;span style=&quot;left:105.963px;top:808.632px;14.9711px;serif;transform:scaleX(1.02139);&quot;&gt;sion severity classes; low, moderate, high and very high severi&lt;/span&gt;&lt;span style=&quot;left:487.32px;top:808.632px;14.9711px;serif;transform:scaleX(1.01543);&quot;&gt;ty representing respectively 40, 30.48, 22.59 and &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:825.845px;14.9711px;serif;transform:scaleX(1.01372);&quot;&gt;6.89% of the total surface. The a&lt;/span&gt;&lt;span style=&quot;left:303.993px;top:825.845px;14.9711px;serif;transform:scaleX(1.00953);&quot;&gt;reas, showing moderate, high a&lt;/span&gt;&lt;span style=&quot;left:491.893px;top:825.845px;14.9711px;serif;transform:scaleX(1.00919);&quot;&gt;nd very high erosion rates which represent more &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:842.967px;14.9711px;serif;transform:scaleX(1.0084);&quot;&gt;than half of the basin area were found generally located in reg&lt;/span&gt;&lt;span style=&quot;left:480.148px;top:842.967px;14.9711px;serif;transform:scaleX(1.00558);&quot;&gt;ions having high erodibility soils, steep slopes and &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:860.179px;14.9711px;serif;transform:scaleX(1.01828);&quot;&gt;low vegetation cover. These areas should be considered as prior&lt;/span&gt;&lt;span style=&quot;left:494.403px;top:860.179px;14.9711px;serif;transform:scaleX(1.01575);&quot;&gt;ities in future erosion control programs in order &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:877.392px;14.9711px;serif;transform:scaleX(0.998794);&quot;&gt;to decrease the siltation rate&lt;/span&gt;&lt;span style=&quot;left:272.795px;top:877.392px;14.9711px;serif;transform:scaleX(1.00459);&quot;&gt; in the Cheffia reservoir. &lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">No. 36 (I–III)</style></issue></record></records></xml>