Soru

Zorluk: ZorSoil Types, Distribution, and Soil Conservation in Nigeria

Match each soil conservation and management strategy implemented in Nigeria on the left with the corresponding soil degradation threat and soil type it primarily addresses on the right.

  • Establishment of multi-row shelterbelts and afforestation belts across Sokoto, Katsina, and Kano statesControl of wind erosion, sand dune drift, and moisture loss on loose, sandy northern Regosols and brown soils
  • Installation of gabion check dams, drainage diversions, and bamboo revegetation along the Agulu-Nanka and Enugu escarpmentsMitigation of catastrophic gully incision and severe structural breakdown in friable, deeply weathered, sandy Ferrallitic soils
  • Implementation of stone terracing, contour ridging, and strip cropping on the elevated slopes of the Jos PlateauPrevention of extensive sheetwash, surface runoff erosion, and topsoil loss on thin, basement-derived Ferruginous soils
  • Construction of protective dykes, tidal bunds, and controlled drainage systems across the coastal lowlands of the Niger DeltaManagement of tidal flooding, salinization, and prolonged waterlogging in coastal Hydromorphic and mangrove swamp soils

Cevap

The correct pairings match each regional soil conservation practice in Nigeria to its target soil type and degradation mechanism: Shelterbelts in northern states control wind erosion on loose Regosols; Gabion check dams and revegetation in Southeastern escarpments stabilize deep gully erosion on friable sandy Ferrallitic soils; Terracing and contour ridging on the Jos Plateau prevent sheet erosion on shallow highland Ferruginous soils; Dykes and drainage controls in the Niger Delta manage tidal flooding and salinization in coastal Hydromorphic soils.
Each pair correctly links a distinct Nigerian geographic region and soil conservation method with its specific soil degradation process and soil group. Shelterbelts stabilize light-textured northern Regosols against wind erosion; gabions and biological planting remediate catastrophic gully erosion in deep Southeastern sandy Ferrallitic soils; stone terracing limits sheet erosion on Jos Plateau Ferruginous soils; and coastal bunds manage flooding/salinization in Niger Delta Hydromorphic soils.

Adım Adım Çözüm

1
Analyze Northern Nigerian environmental conditions and soil conservation responses.
In semi-arid states like Sokoto, Katsina, and Kano, dry harmattan winds induce wind erosion on loose, coarse-textured Regosols. Multi-row shelterbelts serve as physical barriers that reduce wind speed and retain soil moisture.
Matching shelterbelts to wind erosion control on northern sandy soils.
2
Evaluate soil degradation dynamics in Southeastern Nigeria.
Southeastern Nigeria (e.g., Agulu-Nanka in Anambra, Enugu) features deep, weakly structured sandy Ferrallitic soils on steep escarpments. High rainfall energy causes rapid gully incision, requiring mechanical structures like gabion check dams alongside deep-rooted biological cover (bamboo).
Matching escarpments and gully control structures to sandy Ferrallitic soils.
3
Examine highland slope management on the Jos Plateau.
The Jos Plateau experiences intense seasonal rainfall on sloping terrain underlain by thin Ferruginous tropical soils over crystalline basement rocks. Stone terracing and contour ridging break the slope length and slow water velocity to minimize sheetwash.
Matching highland terracing to sheet erosion control on Ferruginous soils.
4
Assess coastal soil management in the Niger Delta.
The low-lying Niger Delta consists of Hydromorphic and mangrove soils subject to daily tides, seasonal inundation, and saline intrusion. Dykes, tidal bunds, and managed drainage prevent coastal erosion and soil degradation due to excess salinity.
Matching coastal engineering controls to Hydromorphic and mangrove soil hazards.

Anahtar Kavram

Regional variation of soil degradation mechanisms and targeted soil conservation techniques across Nigerian soil zones
Tahmini Süre:2m 0s
Bu soruyu puanla