Flood variation and soil nutrient content in floodplain vegetation communities in the Okavango Delta

We investigated the influence of hydroperiod variation on soil nutrient content in the Okavango Delta seasonal floodplains. Soil samples were collected from eight zones of homogenous vegetation cover after low and high floods and analysed for pH, Na, Mg, Ca, K and P content. A Student's t -...

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Main Authors: Gaolathe Tsheboeng, Mphaphi Bonyongo, Mike Murray-Hudson
Format: Article
Language:English
Published: Academy of Science of South Africa 2017-12-01
Series:South African Journal of Science
Subjects:
Online Access:https://www.sajs.co.za/article/view/3766
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author Gaolathe Tsheboeng
Mphaphi Bonyongo
Mike Murray-Hudson
author_facet Gaolathe Tsheboeng
Mphaphi Bonyongo
Mike Murray-Hudson
author_sort Gaolathe Tsheboeng
collection DOAJ
description We investigated the influence of hydroperiod variation on soil nutrient content in the Okavango Delta seasonal floodplains. Soil samples were collected from eight zones of homogenous vegetation cover after low and high floods and analysed for pH, Na, Mg, Ca, K and P content. A Student's t -test was used to test for differences in pH, Na, Mg, Ca, K and P between soils after low and high floods. The Kruskal-Wallis test was used to compare means of flooding duration and depth between low and high floods. Na, K, Mg, P and pH levels in soils were significantly different ( p <0.05) after low floods compared with after high floods. Na content was lower ( p <0.05) in Zones 2 and 8 and higher ( p <0.05) in Zones 4, 5 and 6 during high flood than during low flood. Ca content was lower ( p <0.05) in Zones 1, 2, 3, 4 and 5 and higher in Zone 7 ( p <0.05) under high flood than during low flood. Mg content was lower ( p <0.05) in Zones 1 and 5 and higher ( p <0.05) in Zones 6, 7 and 8 during high flood than during low flood. K content was lower in Zones 1 and 3 and lower in Zones 6, 7 and 8 ( p <0.05) during high flood than during low flood. pH was significantly lower and higher after a high flood in Zones 1 and 6, respectively, than during low flood. P content was significantly ( p <0.05) higher in all zones after high flood than after low flood. Flooding depth and duration increased ( p <0.05) in all vegetation zones during high flood. Our results have direct implications for molapo (flood recession) farming. We recommend that farmers plough immediately after the onset of flood recession when the soil is still moist and rich in nutrients.
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spelling doaj.art-e4480fb4feab4599b76495d64aef460a2022-12-21T18:27:38ZengAcademy of Science of South AfricaSouth African Journal of Science1996-74892017-12-011103/41510.1590/sajs.2014/201301683766Flood variation and soil nutrient content in floodplain vegetation communities in the Okavango DeltaGaolathe Tsheboeng0Mphaphi Bonyongo1Mike Murray-Hudson2Okavango Research Institute, Maun, BotswanaOkavango Research Institute, Maun, BotswanaOkavango Research Institute, Maun, BotswanaWe investigated the influence of hydroperiod variation on soil nutrient content in the Okavango Delta seasonal floodplains. Soil samples were collected from eight zones of homogenous vegetation cover after low and high floods and analysed for pH, Na, Mg, Ca, K and P content. A Student's t -test was used to test for differences in pH, Na, Mg, Ca, K and P between soils after low and high floods. The Kruskal-Wallis test was used to compare means of flooding duration and depth between low and high floods. Na, K, Mg, P and pH levels in soils were significantly different ( p <0.05) after low floods compared with after high floods. Na content was lower ( p <0.05) in Zones 2 and 8 and higher ( p <0.05) in Zones 4, 5 and 6 during high flood than during low flood. Ca content was lower ( p <0.05) in Zones 1, 2, 3, 4 and 5 and higher in Zone 7 ( p <0.05) under high flood than during low flood. Mg content was lower ( p <0.05) in Zones 1 and 5 and higher ( p <0.05) in Zones 6, 7 and 8 during high flood than during low flood. K content was lower in Zones 1 and 3 and lower in Zones 6, 7 and 8 ( p <0.05) during high flood than during low flood. pH was significantly lower and higher after a high flood in Zones 1 and 6, respectively, than during low flood. P content was significantly ( p <0.05) higher in all zones after high flood than after low flood. Flooding depth and duration increased ( p <0.05) in all vegetation zones during high flood. Our results have direct implications for molapo (flood recession) farming. We recommend that farmers plough immediately after the onset of flood recession when the soil is still moist and rich in nutrients.https://www.sajs.co.za/article/view/3766floodcommunitiessoilvegetationzones
spellingShingle Gaolathe Tsheboeng
Mphaphi Bonyongo
Mike Murray-Hudson
Flood variation and soil nutrient content in floodplain vegetation communities in the Okavango Delta
South African Journal of Science
flood
communities
soil
vegetation
zones
title Flood variation and soil nutrient content in floodplain vegetation communities in the Okavango Delta
title_full Flood variation and soil nutrient content in floodplain vegetation communities in the Okavango Delta
title_fullStr Flood variation and soil nutrient content in floodplain vegetation communities in the Okavango Delta
title_full_unstemmed Flood variation and soil nutrient content in floodplain vegetation communities in the Okavango Delta
title_short Flood variation and soil nutrient content in floodplain vegetation communities in the Okavango Delta
title_sort flood variation and soil nutrient content in floodplain vegetation communities in the okavango delta
topic flood
communities
soil
vegetation
zones
url https://www.sajs.co.za/article/view/3766
work_keys_str_mv AT gaolathetsheboeng floodvariationandsoilnutrientcontentinfloodplainvegetationcommunitiesintheokavangodelta
AT mphaphibonyongo floodvariationandsoilnutrientcontentinfloodplainvegetationcommunitiesintheokavangodelta
AT mikemurrayhudson floodvariationandsoilnutrientcontentinfloodplainvegetationcommunitiesintheokavangodelta