@article{fdi:010077476, title = {{C}ontribution of time domain electromagnetic and magnetic resonance soundings to groundwater assessment at the margin of lake {C}had basin, {C}ameroon}, author = {{K}emgang {D}ongmo, {T}. and {B}oucher, {M}arie and {M}vondo, {V}.{Y}.{E} . and {F}avreau, {G}uillaume and {N}gounou {N}gatcha, {B}. and {Y}alo, {N}. and {G}oni, {I}.{B}. and {L}egchenko, {A}natoli}, editor = {}, language = {{ENG}}, abstract = {{A}t the edge of a semi-arid sedimentary basin, the {P}iedmont plain of the {M}andara mountains is potentially a key area for the recharge of the {L}ake {C}had {Q}uaternary aquifer. {W}e conducted two geophysical surveys based on magnetic resonance sounding ({MRS}) and {T}ime-{D}omain {E}lectromagnetism ({TDEM}) techniques for a better understanding of the aquifer structure at.the piedmont scale in aim to identify preferential groundwater recharge pathways. {MRS} water content and electrical resistivity of the medium confirmed the very heterogeneous and clayey nature of the quaternary aquifer, limiting the recharge to the sandiest areas. {T}hanks to the geophysical methods, these areas have been highlighted near temporary rivers and upstream of the study area near {M}aroua city. {B}ecause of the thickening of the aquifer downstream, the most transmissive zones are in the mid-slope of the piedmont. {T}he geographical distribution of aquifer properties defined by geophysics and the range of {MRS} water content (from <2% to 26%) may be used in the future to constrain groundwater modelling and specify the recharge of the quaternary aquifer at mountain front.}, keywords = {{G}roundwater resources ; {M}ountain front recharge ; {P}iedmont aquifer ; {S}emi-arid climate ; {TDEM} / {MRS} ; {W}est and {C}entral {A}frica ; {CAMEROUN} ; {MANDARA} {MONTS} ; {MAROUA} ; {TCHAD} {LAC} {BASSIN}}, booktitle = {}, journal = {{J}ournal of {A}pplied {G}eophysics}, volume = {170}, numero = {}, pages = {art. 103840 [10 p.]}, ISSN = {0926-9851}, year = {2019}, DOI = {10.1016/j.jappgeo.2019.103840}, URL = {https://www.documentation.ird.fr/hor/fdi:010077476}, }