Soil water erosion is recognized as the principal mechanisms behind soil organic carbon
(SOC) losses from soils, a soil constituent essential for ecosystem functions. SOC erosion can
thus be far-reaching, affecting the future human welfare and the sustainability of ecosystems.
Little research has yet been done to investigate the main mechanisms involved in the lateral
translocation of SOC on the landscape. Understanding the effects of the different water
erosion mechanisms, which control SOC losses (SOCL) at the hillslope level, creates scope
for further scientific studies.
Empirical data from 357 plots, with a range in slope length from 1 (n=117) to 22.1m (n=240)
were analysed to estimate the global variations of particulate organic carbon content (POCC),
POC losses (POCL) and sediment POC enrichment ratio (ER). The global average POCL rate
was calculated to be 12.1 g C m-2 y-1. Tropical clayey soil environments revealed the highest
POCL (POCL=18.0 g C m-2 y-1), followed by semi-arid sandy (POCL=16.2 g C m-2 y-1) and
temperate clayey soil environments (POCL=2.9 g C m-2 y-1). The global net amount of SOC
displaced from its original bulk soil on an annual basis was calculated to be 0.59±0.09 Gt C,
making up an approximated 6.5% of the net annual fossil fuel induced C emissions (9 Gt C).
POCL data for different spatial scales revealed that up to 83% of the eroded POC re-deposits
near its origin in hillslopes, and is not exported out of the catchment. The low organic carbon
sediment ER obtained from the data of clayey soils (ER of 1.1) suggests that most of the
eroded POC remains protected within soil aggregates. Consequently, erosion-induced carbon
dioxide (CO2) emissions in tropical areas with clayey soils are likely to be limited (less than
10%), as the process of POC re-burial in hillslopes is likely to decrease the rate of organic
matter (OM) decomposition and thus serve as a potential carbon sink. Water erosion in sandy
and silty soils revealed organic carbon sediment ER as high as 3.0 and 5.0, suggesting that in
these soils the eroded POC is not re-buried, but is made vulnerable to micro-decomposers,
thus adding to the atmospheric CO2 influx. The results obtained in the review study only
reaffirm that large variations of POCL are evident across the different pedo-climatic regions
of the world, making it a scientific imperative to conduct further studies investigating the link
between SOC erosion by water and the global carbon cycle.
A field study was designed to quantify the POC exported in the eroded sediments from
1x1m2 and 2x5m2 erosion plots, installed at different hillslope aspects, and to further identify
the main erosion mechanisms involved in SOC erosion and the pertaining factors of control.
The erosion plots were installed on five topographic positions under different soil types,
varying vegetation cover, and geology in the foothills of the Drakensberg mountain range of
South Africa. Soil loss (SL), sediment concentration (SC), runoff water (R) and POCL data
were obtained for every rainfall event from November 2010 up to February 2013. Scale ratios
were calculated to determine which erosion mechanism, rain-impacted flow versus raindrop
erosion, dominates R, SL and POCL. Averaged out across the 32 rainfall events, there were
no significant differences in R and POCL between the two plot sizes but SL were markedly
higher on the 5m compared to the 1m erosion plots (174.5 vs 27g m-1). This demonstrates that
the sheet erosion mechanism has a greater efficiency on longer as opposed to shorter slopes.
Rain-impacted flow was least effective where soils displayed high vegetation coverage (P <
0.05) and most efficient on steep slopes with a high prevalence of soil surface crusting. By
investigating the role of scale in erosion, it was possible to single out the controlling in situ
(soil surface related conditions) and ex situ (rainfall characteristics) involved in the export of
SOC from soils. This information will in future contribute toward generating SOC specific
models and thus further inform erosion mitigation. / M. Sc. University of KwaZulu-Natal, Durban 2013.
| Identifer | oai:union.ndltd.org:netd.ac.za/oai:union.ndltd.org:ukzn/oai:http://researchspace.ukzn.ac.za:10413/11424 |
| Date | January 2013 |
| Creators | Müller-Nedebock, Daniel |
| Contributors | Chaplot, Vincent A. M., Chivenge, Pauline |
| Source Sets | South African National ETD Portal |
| Language | en_ZA |
| Detected Language | English |
| Type | Thesis |
Page generated in 0.0024 seconds