03 — Geology & soilsJiolojia na udongo
What lies under the field
Kilichopo chini ya shamba
The site sits on a Cenozoic sequence — shales, quartzites, gneisses and granitic rocks. The surface layer is a grey, sandy, shale-derived soil, interfingered with the heavier mbuga clays typical of the low-lying depressions of central Tanzania.
Eneo lipo juu ya mfumo wa Cenozoic — shale, quartzite, gneiss na mawe ya granite. Tabaka la juu ni udongo wa kijivu, wa kichanga, unaotokana na shale, uliochanganyika na udongo mzito wa mbuga unaopatikana katika mabonde ya Tanzania ya kati.
This combination is workable but demanding. The sandy fraction drains and heats quickly and is prone to blowing when bare; the mbuga clays hold water well but seal and crack, and must be worked at the right moisture. Both argue for less inversion, more cover, and deeper rooting.
Mchanganyiko huu unalimika lakini unahitaji uangalifu. Sehemu ya kichanga hupitisha maji na kupata joto haraka na hupeperushwa na upepo ikiwa wazi; udongo wa mbuga huhifadhi maji vizuri lakini hujifunga na kupasuka, na unapaswa kulimwa kwa unyevu unaofaa. Vyote vinashauri kupindua udongo kidogo, kifuniko zaidi, na mizizi ya kina.