Abstract:
Soil is the largest terrestrial carbon storage; it contains carbon as much as three times of plant
biomass and two times of the atmosphere. Surface layer is the most fertile zone which is rich in
organic matter. However, this fertile zone is degraded from rough land management, and also
removed by heavy rain, which is considered as the effect of climate change. The typical
characteristics of these degraded soils are poor in infiltration. Lack of organic matter fails to
create soil aggregates and surface crust tends to be formed at the surface soils. Traditional
countermeasure for this situation in cultivation is soil turn over. It makes soil layer softer,
agricultural jobs easier and enhances infiltration. However, it may also break soil aggregates and
make soils drier, which would be a cause of erosion and loss of organic matter. X-ray CT images
of the natural soils showed that root created macropores were predominant. The tubular pore
networks helps water and solute movement. Therefore, artificial macropores were installed in
degraded red-yellow soils to enhance vertical infiltration without cultivation. Fibrous materials
were inserted in the macropores to reinforce its structure while enhancing infiltration with their
capillary force. Macropores and control (no macropore) plots were established and bulk density,
hydraulic conductivity, plant biomass and total carbon in soil were measured. The results after
one-year macropores installation were that bulk density was lower and hydraulic conductivity
was relatively higher at macropores plot than that of the control plot. In addition, plant biomass
and total carbon were larger at macropores plot. There was a concern that introduced fresh
water with nutrient and oxygen would decompose organic matter. However, enhancing
infiltration along with naturally occurred nutrient would positively affect plant growth which
subsequently helps carbon storage in soils.
