Other language title :
مقدار كربن آلي خاك و رابطه بين ميزان آن و مديريت چرا در مراتع نيمه خشك كنيا
Title of article :
Soil Organic Carbon Content and Stocks in Relation to Grazing Management in Semi-Arid Grasslands of Kenya
Author/Authors :
Rotich, Hillary Kipngetich Department of Land Resource and Agricultural Technology - University of Nairobi - Nairobi, Kenya , Onwonga, Richard Department of Land Resource and Agricultural Technology - University of Nairobi - Nairobi, Kenya , Mbau, Judith Syombua Department of Land Resource and Agricultural Technology - University of Nairobi - Nairobi, Kenya , Koech, Oscar Kipchirchir Department of Land Resource and Agricultural Technology - University of Nairobi - Nairobi, Kenya
Abstract :
Rangelands cover approximately 85% of Kenya’s land mass and is a major
resource for livestock farming with a considerable potential to mitigate climate change, yet
these lands are stressed differently by various management. Our study aimed at
determining the influence of grazing management systems (rotational, continuous and
ungrazed) on soil organic carbon stocks in Yoani ranch located in the southern rangelands
of Kenya (2016). This research was conducted on a commercial grazing ranch, a section of
it was converted from continuous grazing into rotational grazing and has been under
rotational grazing for 11 years during the time the research was conducted. Within the
same ranch, there was a section with similar geomorphology and soils as the rotationally
grazed which was not converted and has been continuously grazed for over 30 years to
represent the continuous grazing system. The ungrazed area consists of an abandon section
of the ranch for more than 30 years due to a deep gully which was formed by gully erosion
creating an isolated area inaccessible by livestock. Soil samples were taken up to a depth of
1.2m, at an interval of 0-10, 10-20 cm, 20-30 cm, 30-60 cm, 60-90 cm and 90-120 cm. The
difference between soil sampling depths is because the upper layer between 0-30 cm is
more dynamic with respect to soil microbial activities which can be influenced by grazing
as compared to the deeper depths along the soil profile. The ungrazed site recorded
significantly (P<0.5) higher soil organic carbon concentrations than rotational and
continuously grazed sites for all soil layers up to 1.2m depth. The rotationally grazed site
had higher soil organic carbon concentrations across depths compared to continuously
grazing system which was attributed to grazing management effects.
Farsi abstract :
ﭼﮑﯿﺪه. ﻣﺮاﺗﻊ ﮐﻨﯿﺎ ﺣﺪود 85 درﺻﺪ از اراﺿﯽ ﮐﺸﻮر را ﭘﻮﺷﺶ ﻣﯽدﻫﺪ و ﻣﻨﺒﻊ اﺻﻠﯽ ﺑﺮاي داﻣﺪاري اﺳﺖ ﮐﻪ ﭘﺘﺎﻧﺴﯿﻞ ﻗﺎﺑﻞ ﺗﻮﺟﻬﯽ ﺑﺮاي ﻣﻘﺎﺑﻠﻪ ﺑﺎ ﺗﻐﯿﯿﺮات آب و ﻫﻮاﯾﯽ دارد، ﺑﺎ اﯾﻦ ﺣﺎل، اﯾﻦ ﻣﻨﺎﻃﻖ ﺗﺤﺖ ﺗﺎﺛﯿﺮ ﻣﺪﯾﺮﯾﺖ و ﻓﺸﺎرﻫﺎي ﻣﺨﺘﻠﻒ ﻗﺮار ﮔﺮﻓﺘﻪ اﺳﺖ. ﻣﻄﺎﻟﻌﻪ ﺣﺎﺿﺮ ﺑﺎ ﻫﺪف ﺗﻌﯿﯿﻦ ﺗﺄﺛﯿﺮ ﺳﯿﺴﺘﻢﻫﺎي ﻣﺪﯾﺮﯾﺖ ﭼﺮاي )ﭼﺮﺧﺸﯽ، ﻣﺪاوم و ﺑﺪون ﭼﺮا( ﺑﺮ ذﺧﺎﺋﺮ ﮐﺮﺑﻦ آﻟﯽ ﺧﺎك در ﻣﺮاﺗﻊ ﺗﺠﺎري ﯾﻮاﻧﯽ، واﻗﻊ در ﻣﺮاﺗﻊ ﺟﻨﻮب ﮐﻨﯿﺎ در ﺳﺎل 1395 اﻧﺠﺎم ﺷﺪ. ﺑﺨﺸﯽ از اﯾﻦ ﻣﺮاﺗﻊ ﺗﺤﺖ ﻣﺪﯾﺮﯾﺖ ﭼﺮاي ﻣﺴﺘﻤﺮ و ﺑﺨﺸﯽ ﺑﻪ ﭼﺮاي ﭼﺮﺧﺸﯽ ﺑﻪ ﻣﺪت 11 ﺳﺎل ﺑﺮاي اﻧﺠﺎم ﺗﺤﻘﯿﻘﺎت ﻣﻮرد اﺳﺘﻔﺎده ﻗﺮار ﮔﺮﻓﺖ. در ﻫﺮ دو ﺗﯿﻤﺎر ﭼﺮاي ﻣﺴﺘﻤﺮ و ﭼﺮاي ﭼﺮﺧﺸﯽ ﺷﺮاﯾﻂ ﺧﺎﮐﯽ و زﻣﯿﻦﺷﻨﺎﺳﯽ ﯾﮑﺴﺎن ﺑﻮد و در ﺑﺨﺶ ﭼﺮاي ﻣﺴﺘﻤﺮ ﺑﻪ ﻣﺪت ﺑﯿﺶ از 30 ﺳﺎل ﺑﺮاي ﻧﺸﺎن دادن اﺛﺮ آن ﺑﺮ ﻣﯿﺰان ﮐﺮﺑﻦ آﻟﯽ ﺧﺎك ﻣﻮرد اﺳﺘﻔﺎده ﻗﺮار ﮔﺮﻓﺖ. در ﺑﺨﺸﯽ از ﻣﺮاﺗﻊ اﯾﻦ ﻣﻨﻄﻘﻪ ﮔﺎﻟﯽ ﯾﺎ ﺧﻨﺪق ﻋﻤﯿﻘﯽ ﻗﺮار دارد ﮐﻪ ﺑﯿﺶ از 30 ﺳﺎل اﺳﺖ ﻏﯿﺮ ﻗﺎﺑﻞ ﭼﺮا ﺷﺪه اﺳﺖ. ﻧﻤﻮﻧﻪﻫﺎي خاك تا عمق ﻣﺘﺮي ﺑﺮداﺷﺖ ﺷﺪﻧﺪ از ﻋﻤﻖﻫﺎي 120 و 60-90 ،30-60 ،20-30 ،10-20 ،0-10. 90 ﺳﺎﻧﺘﯽﻣﺘﺮي ﻧﻤﻮﻧﻪﻫﺎي ﺧﺎك ﺟﻤﻊآوري ﺷﺪﻧﺪ. ﺗﻔﺎوت ﺑﯿﻦ ﻋﻤﻖ ﻧﻤﻮﻧﻪﺑﺮداري از ﺧﺎك ﺑﻪ اﯾﻦ دﻟﯿﻞ اﺳﺖ ﮐﻪ در ﻻﯾﻪ ﺑﺎﻻﯾﯽ ﯾﻌﻨﯽ ﺑﯿﻦ 0 ﺗﺎ 30 ﺳﺎﻧﺘﯽ ﻣﺘﺮ ﻓﻌﺎﻟﯿﺖﻫﺎي ﻣﯿﮑﺮوﺑﯽ ﺧﺎك ﺑﯿﺸﺘﺮ اﺳﺖ ﮐﻪ ﻣﯽﺗﻮاﻧﺪ ﺗﺤﺖ ﺗﺄﺛﯿﺮ ﭼﺮاي ﺑﯿﺸﺘﺮ در ﻣﻘﺎﯾﺴﻪ ﺑﺎ ﻗﺴﻤﺖﻫﺎي ﻋﻤﯿﻖ ﺧﺎك ﻗﺮار ﮔﯿﺮد. ﻧﺘﺎﯾﺞ ﻧﺸﺎن داد ﮐﻪ در ﺗﯿﻤﺎر ﻓﺮﺳﺎﯾﺶ ﯾﺎﻓﺘﻪ ﺑﻪ ﻃﻮر ﻣﻌﻨﯽداري )P<0.5( ﺑﯿﺸﺘﺮﯾﻦ ﻣﯿﺰان ﻏﻠﻈﺖ ﮐﺮﺑﻦ آﻟﯽ ﺧﺎك در ﺗﻤﺎم ﻻﯾﻪﻫﺎي ﺧﺎك ﺗﺎ ﻋﻤﻖ 1/2 ﻣﺘﺮي ﻧﺴﺒﺖ ﺑﻪ ﺗﯿﻤﺎرﻫﺎي ﭼﺮاي ﻣﺪاوم و ﭼﺮاي ﭼﺮﺧﺸﯽ ﻧﺸﺎن ﻣﯽدﻫﺪ. ﻫﻤﭽﻨﯿﻦ در ﺗﯿﻤﺎر ﺑﺎ ﭼﺮاي ﭼﺮﺧﺸﯽ، ﻏﻠﻈﺖ ﮐﺮﺑﻦ آﻟﯽ ﺧﺎك در ﻗﺴﻤﺖﻫﺎي ﻋﻤﯿﻖ در ﻣﻘﺎﯾﺴﻪ ﺑﺎ ﺳﯿﺴﺘﻢ ﭼﺮاي ﻣﺪاوم ﺑﯿﺸﺘﺮ ﺑﻮد ﮐﻪ اﯾﻦ ﻣﻮﺿﻮع ﺷﺎﯾﺪ ﺑﻪ دﻟﯿﻞ اﺛﺮات ﻣﺪﯾﺮﯾﺖ ﭼﺮاﮔﺎه ﺑﺎﺷﺪ.
Keywords :
Rangelands , Grazing systems , Soil organic carbon stocks
Journal title :
Astroparticle Physics