<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222020000200012</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2020v72n2a290719</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Alteraciones en el cauce del río Seco y pérdidas de tierras agrícolas, provincia de Tucumán, Argentina]]></article-title>
<article-title xml:lang="en"><![CDATA[Alterations in the Seco river bed and losses of agricultural land, province of Tucumán, Argentina]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Toledo]]></surname>
<given-names><![CDATA[Mario Arnaldo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ahumada]]></surname>
<given-names><![CDATA[Ana Lía]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ibañez Palacios]]></surname>
<given-names><![CDATA[Gloria Patricia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Instituto de Geología de Cuaternario y Paleoclimas  ]]></institution>
<addr-line><![CDATA[San Miguel de Tucumán Tucumán]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,IGCYP FML ]]></institution>
<addr-line><![CDATA[San Miguel de Tucumán Tucumán]]></addr-line>
<country>Argentina</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<volume>72</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222020000200012&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222020000200012&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222020000200012&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La provincia de Tucumán, Argentina, presenta una densa red fluvial, con ríos que han manifestado, en los últimos 45 años, comportamientos complejos y dinámicos a consecuencia de los elevados caudales que les son aportados por sus cuencas superiores. En estas cuencas, ubicadas en la zona montañosa y pedemontana, se desarrollan diversas actividades antrópicas en relieves contrastados, con pendientes erosivas. El incremento de las precipitaciones registrado en la región a partir del año 1970 ha acrecentado los procesos erosivos y deposicionales en la llanura aluvial, modificando el diseño de los cauces, con importantes consecuencias sobre los campos de cultivo. Se analiza el cauce del río Seco, el cual tiene sus nacientes en la ladera oriental de la Sierra del Aconquija, recorre el piedemonte y la llanura aluvial en sentido Oeste-Este, hasta desaguar en el río Salí; cauce principal del sistema hídrico de la provincia. El principal objetivo de este trabajo fue realizar el análisis morfológico de los meandros en un tramo de su cauce, de aproximadamente 6.28 km de longitud, para el lapso temporal 1972 - 2017. Se analizó: la sinuosidad del cauce y los procesos de cortes de meandros por desborde (chute cutoff) y por tangencia (neck cutoff). Estos procesos han generado la pérdida acelerada de tierras agrícolas por erosión lateral de las barrancas del río, compuestas por sedimentos fluvio-aluviales, materiales parentales de los suelos productivos de la llanura aluvial. Previamente, se resaltan las características generales de la cuenca del río Seco, considerando la geología, geomorfología, clima, suelos y actividades antrópicas. También las características específicas de la subcuenca que aporta sus aguas al tramo meandriforme, principalmente: el incremento de los caudales por el cambio de uso de los suelos, las pendientes del terreno, la región geomorfológica y la morfometría. Para el mapeo del cauce y de los cultivos se emplearon imágenes satelitales Landsat y Sentinel, y con el Modelo de Elevación Digital SRTM se elaboraron los mapas de: divisorias de aguas de la cuenca y de la subcuenca de aporte a los meandros, pendientes, curvas de nivel y red de drenaje. Los resultados muestran que la sinuosidad del cauce se incrementó en el lapso temporal 1972 -2002, tuvo una notable disminución en el lapso temporal 2002-2011 por los procesos de corte de meandros, incrementándose nuevamente en el lapso temporal 2011-2017, conjuntamente con la migración del cauce hacia el cuadrante sur. Estos cambios produjeron la pérdida de 370.68 ha de suelos productivos, lo que constituye 7.41 hm3 de sedimentos removidos y transportados por la corriente. Los meandros del río Seco reflejan la degradación de la subcuenca de aporte, representando la situación de las cuencas del Noroeste Argentino, en las cuales el incremento en la intensidad y frecuencia de las precipitaciones a partir del año 1970 han generado condiciones críticas, cuyos efectos son más evidentes en las áreas bajas.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The province of Tucumán, Argentina has a dense fluvial network, with rivers that have shown, over the last 45 years, complex and dynamic behaviors, as a result of high streamflows. In the upper basins, located in the mountainous zone and piedmont, diverse anthropic activities developed in contrasted reliefs and erosive slopes. The increase in rainfall recorded in the region since 1970 has increased both the erosive and depositional processes in the alluvial plain by modifying the design of the channels, with important consequences on the farmlands. In this paper, the Seco river bed is analyzed thoroughly. The Seco river is born on the eastern slope of the Aconquija mountains, runs through the piedmont and the alluvial plain in a west-east direction, and finally discharges into the Salí river, the main river bed of the fluvial network of the province. The main objective of this work is an analysis of meander morphology along 6.28 km of the Seco river for the period 1972 to 2017. The main parameters analyzed were the sinuosity of the channel, and meander cuts by overflow (chute cutoff) and by tangency (neck cutoff). These processes have accelerated the loss of agricultural land by lateral erosion on the river ravines, which are composed of fluvial-alluvial sediments, the parental materials of the productive soils of alluvial plains. To begin our study, the general characteristics of the Seco river basin have been considered, including geology, geomorphology, climate, soils, and anthropic activities. In addition, specific features of the sub-basin that contributes its waters to the meander section were also taken into account: the increase of the flows due to the change toward the use of surrounding soils, the slopes of the field, the geomorphological region and morphometry. Landsat and Sentinel satellite images, as well as the SRTM Digital Elevation Model (DEM), were used for mapping the channel and crops. The resulting maps are basin and sub-basin watershed contribution to the meanders, slopes, elevation curves, and drainage network. The results show that the sinuosity of the channel increased in the period 1972-2002, had a notable decrease in the period 2002-2011 due to the processes of meander cuts, and increased again in the period 2011-2017, together with the migration of the channel towards the southern quadrant. These changes resulted in the loss of 370.68 ha of productive soils, which represents 7.41 hm3 of sediments removed and transported by the current. The meanders of the Seco river reflect the degradation of its area of contribution, representing the situation of the basins of the Argentine Northwest, in which the increase in the intensity and frequency of the precipitations since 1970 have generated critical conditions, whose effects are more evident in low areas.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[río Seco]]></kwd>
<kwd lng="es"><![CDATA[meandros]]></kwd>
<kwd lng="es"><![CDATA[imágenes satelitales]]></kwd>
<kwd lng="es"><![CDATA[uso del suelo]]></kwd>
<kwd lng="es"><![CDATA[precipitaciones]]></kwd>
<kwd lng="es"><![CDATA[Argentina]]></kwd>
<kwd lng="en"><![CDATA[Seco river]]></kwd>
<kwd lng="en"><![CDATA[meander]]></kwd>
<kwd lng="en"><![CDATA[satellite image]]></kwd>
<kwd lng="en"><![CDATA[land use]]></kwd>
<kwd lng="en"><![CDATA[rainfall]]></kwd>
<kwd lng="en"><![CDATA[Argentina]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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