Publications des scientifiques de l'IRD

Prat Christian. (1997). Analisis de las caracteristicas de las precipitaciones de 1992 a 1995 en San Miguel Tlaixpan (Texcoco, Mexico). In : Zebrowski Claude (ed.), Quantin Paul (ed.), Trujillo G. (ed.), Villamar M.D. (collab.). Suelos volcanicos endurecidos. Quito (ECU) ; Quito (ECU) ; Quito (ECU) ; Quito : UE ; ORSTOM ; PUCE ; UCE, p. 359-370. Suelos Volcanicos Endurecidos, 3., Quito (ECU), 1996/12/9-14.

Titre du document
Analisis de las caracteristicas de las precipitaciones de 1992 a 1995 en San Miguel Tlaixpan (Texcoco, Mexico)
Année de publication
1997
Type de document
Colloque
Auteurs
Prat Christian
In
Zebrowski Claude (ed.), Quantin Paul (ed.), Trujillo G. (ed.), Villamar M.D. (collab.) Suelos volcanicos endurecidos
Source
Quito (ECU) ; Quito (ECU) ; Quito (ECU) ; Quito : UE ; ORSTOM ; PUCE ; UCE, 1997, p. 359-370
Colloque
Suelos Volcanicos Endurecidos, 3., Quito (ECU), 1996/12/9-14
In the UE-ORSTOM-CP-UAT-UG research program about rehabilitation of Mexican tepetates, one of the problems is to control soil erosion and productivity of these new soils. The caracterization of rainfall in relation to its occurence, quantity, energy, etc. is fundamental. This paper shows the results of the analysis of 4 years of precipitations measured with a pluviograph on the study area, and the processing of these data with soft-wares pertaining to ORSTOM (PLUVIOM and ARES). In spite of the short time of the registrations, we could show that the climate is C(w1)(w)-subhumid temperature with an ustic hydric regime in the classification of Koeppen modified by G. Benavides, as other authors have previously showed, but the total precipitation level for the agricultural season is much lower than what was considered: 620mm/year instead of 700/800 mm/year. With this amount of water, we cannot really expect a very corn high production. In relation to the agressivity of the rain, all the rains give a total value of a Rus. Due to the very brief duration of the rains, the maximum intensity during 5,10 or 15 minutes should be taken as a reference instead of 30 minutes to calculate the R coefficient. The variability of the events is very high during the same year and between years, difficulting the comparison of agronomic studies. (Résumé d'auteur).
Plan de classement
Régimes climatiques [062REGHYD02]
Descripteurs
PRECIPITATION ; AGRICULTURE ; AGROCLIMATOLOGIE ; EROSION ; CLIMAT ; METHODOLOGIE ; VARIATION TEMPORELLE ; GEOSTATISTIQUE ; TEPETATE ; ABATTEMENT DE LA PLUIE
Description Géographique
MEXIQUE
Localisation
Fonds IRD [F A010012910] ; Montpellier (Centre IRD)
Identifiant IRD
fdi:010012923
Contact