Hillslope and catchment scale soil organic carbon concentration: An assessment of the role of geomorphology and soil erosion in an undisturbed environment

被引:73
作者
Hancock, G. R. [1 ]
Murphy, D. [2 ]
Evans, K. G. [1 ,3 ]
机构
[1] Univ Newcastle, Sch Environm & Life Sci, Callaghan, NSW 2308, Australia
[2] Univ Western Australia, Sch Earth & Geog Sci, Crawley, WA 6009, Australia
[3] Environm Res Inst Supervising Scientist, Hydrol & Geomorph Proc Program, Darwin, NT, Australia
基金
澳大利亚研究理事会;
关键词
Soil carbon; Soil erosion; Catchment modelling; Hillslope hydrology; Wetness index; Digital elevation model; NORTHERN-TERRITORY; STORAGE PREDICTION; TOTAL NITROGEN; ARNHEM-LAND; LANDSCAPE; DEPOSITION; CS-137; MODELS; MATTER; SASKATCHEWAN;
D O I
10.1016/j.geoderma.2009.11.021
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The role of geomorphology in relation to the spatial and temporal distribution of soil carbon is of considerable interest in terms of landscape management and carbon sequestration. Soil carbon plays an important role in soil water holding capacity, soil structure and overall soil health. Soil is also a significant store of terrestrial carbon. This study examines total soil carbon (SC) concentration at the hillslope and catchment scale in the Tin Camp Creek catchment, Arnhem Land, Northern Territory, Australia. The catchment is largely undisturbed by European agriculture or management practices and is located in the monsoonal tropics. Results show that SC concentration along hillslope transects has remained consistent over a number of years and it is strongly related to hillslope position and topographic factors derived from precision surveying and provides a baseline assessment. Poor relationships were found when using a good quality medium resolution digital elevation model to derive topographic factors. This finding demonstrates the need for high resolution survey data for the prediction of total C at the hillslope and catchment scale. There was little difference in SC concentration between years and overall, SC down the hillslope profile varies little temporally suggesting that concentrations are relatively stable in this environment. An assessment of the relationship between SC and soil erosion using Cs-137 and erosion pins demonstrates that sediment transport and deposition play little role in the distribution of SC in this environment. Vegetative biomass appears to be the major contributor to SC concentration with vegetative biomass being strongly controlled by topographic factors. While the SC concentration is constant over the study period further sampling is required to assess decadal trends. Crown Copyright (C) 2009 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:36 / 45
页数:10
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