Typically, because the heavy nutrient cycling of tropical rain forests are so high, the top soil in these forests is very shallow- perhaps less than a meter. Once the forest is gone and the soil is used for farmland, it will never come back..... then the sun will beat down and further add to the stress of the land------ desert baby yeah.........
One reason is that tropical forests have nutrient-poor soil, which requires intensive and costly fertilization to support agricultural production. Additionally, tropical forests have complex ecosystems that are difficult to replicate in agriculture, leading to higher risks of pest outbreaks and soil degradation.
Typically, because the heavy nutrient cycling of tropical rain forests are so high, the top soil in these forests is very shallow- perhaps less than a meter. Once the forest is gone and the soil is used for farmland, it will never come back..... then the sun will beat down and further add to the stress of the land------ desert baby yeah.........
caecilian
caecilian
Yes but it was rich farmland.
The forests of the taiga, or boreal forests, are less frequently converted into farmland compared to temperate deciduous forests due to several factors. The harsh climate, with long, cold winters and short growing seasons, makes agriculture challenging and less productive. Additionally, the soil in taiga regions is often acidic and nutrient-poor, further limiting agricultural viability. Moreover, the ecological importance of taiga forests and efforts to preserve biodiversity also contribute to their protection from conversion.
most nutrients have been absorbed by the vegetation.
The soil type of Tropical Monsoon Forests is typically laterite soil, which is rich in iron and aluminum oxides, making it nutrient-poor and acidic. These soils are formed through intense weathering due to the heavy rainfall in these regions.
Slash and burn
Because most of the nutrients were absorbed by the vegetation that was removed (trees or other plants), and so cannot be returned to the soil.
The rapid rate of decomposition in tropical forests leads to the quick breakdown of organic matter, which results in low nutrient soil. The warm and humid conditions in tropical forests facilitate the activity of decomposers such as bacteria and fungi, accelerating the recycling of nutrients back into the ecosystem. As a result, the soil in tropical forests tends to be nutrient-poor despite the high biological productivity.
Soil is nutrient-poor and acidic. Decomposition is rapid and soils are subject to heavy leaching.