@article{
 title = {Spatial and Temporal Evolution of the Static Water Level of the Cuauhtemoc Aquifer during the Years 1973, 1991 and 2000: A Geographical Approach},
 type = {article},
 year = {2014},
 identifiers = {[object Object]},
 keywords = {crn3056},
 pages = {572-584},
 volume = {06},
 websites = {http://dx.doi.org/10.4236/jgis.2014.65047,citeulike-article-id:14178931},
 id = {5435633e-2438-35b8-8726-babf59bdf78e},
 created = {2019-04-01T18:02:01.047Z},
 file_attached = {false},
 profile_id = {1f5347e3-dec5-3349-a941-3b484c2dfce9},
 group_id = {184ee5d4-bd93-3566-938b-14cc43849390},
 last_modified = {2019-04-01T18:02:01.047Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {false},
 hidden = {false},
 source_type = {JOUR},
 private_publication = {false},
 abstract = {In hydrogeology it is of great interest to examine the temporal and spatial evolution of aquifers.
      There are different ways of modeling an aquifer: physical models, models based on analog and
      mathematical techniques. Usually, mathematical techniques involve complex operations difficult
      to understand for some people, such as differential or partial equations. In contrast, our method
      requires only a basic knowledge of geometry and trigonometry. Moreover, it is only necessary to
      know the static level of the aquifer at three different dates. Of course, the results may be limited
      compared to those that use advanced mathematical methods; however, our method provides a
      first approximation to determine the behavior of the aquifer through time. Overall, our results allowed
      us to follow the evolution of the aquifer in detail of various areas of increased extraction
      and in which removal has been increasing, but also of areas with a considerable recharge during
      the study period.},
 bibtype = {article},
 author = {Alatorre-Cejudo, L C and Díaz, R E and Miramontes, S and Bravo, L C and Sánchez, E},
 journal = {Journal of Geographic Information System},
 number = {05}
}

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Usually, mathematical techniques involve complex operations difficult\n to understand for some people, such as differential or partial equations. In contrast, our method\n requires only a basic knowledge of geometry and trigonometry. Moreover, it is only necessary to\n know the static level of the aquifer at three different dates. Of course, the results may be limited\n compared to those that use advanced mathematical methods; however, our method provides a\n first approximation to determine the behavior of the aquifer through time. 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