Vegetation cover-abundance and litter accumulation in the humid rain forest of South Eastern Nigeria

GeoJournal ◽  
1990 ◽  
Vol 20 (1) ◽  
pp. 72-73
Author(s):  
Nkanu Eni Edu
1994 ◽  
Vol 45 (8) ◽  
pp. 1509 ◽  
Author(s):  
M Greenway

Litterfall and litter accumulation were investigated over two years in a Melaleuca quinquenewia wetland in south-eastern Queensland. In 1992, a seasonally wet year, litterfall was 809 � 135 g m-2 yr-1 at the floodplain site and 764 �192 g m-2 yr-1 at the riparian site, of which Melaleuca leaf litter made up 65% and 56% respectively. Litterfall was significantly lower and more variable in 1993, a drought year, being 725�106 g m-2 and 675 � 216 g m-2 year-1. There was a distinct seasonal pattern, with peak leaf litterfall occurring in spring in 1992 but extending into summer in 1993. Melaleuca leaf fall was significantly lower in 1993, possibly because drought conditions caused greater leaf longevity. Litter accumulation on the forest floor was 3457 g m-2 at the floodplain site and 2320 g m-2 at the riparian site; there was no significant difference between years, although the organic matter content of the litter was lower in 1992, possibly as a result of leaching during flooding. Carbon content decreased with decreasing particle size of the litter, whereas nitrogen and phosphorus increased. There was no evidence to suggest leaching of nitrogen or phosphorus, and the high C: N: P ratios indicate slow rates of litter decay. The high accumulation of litter mass suggests that these woody wetlands may function as nutrient sinks.


2007 ◽  
Vol 46 (7) ◽  
pp. 754-756 ◽  
Author(s):  
Maurice E. Asuquo ◽  
Pius Agweye ◽  
Gabriel Ugare ◽  
Godwin Ebughe

2020 ◽  
Vol 99 (1-2) ◽  
pp. 13-25
Author(s):  
Mykola Karabiniuk ◽  
Ihor Hnatiak ◽  
Yana Markanych

The results of the study of anthropization of valuable natural territorial complexes of the subalpine and alpine highlands of Chornohora under the influence of recreational and tourist activities in the vicinity of Brebeneskul Lake (Ukrainian Carpathians) are presented. Anthropization is caused by continuous cutting of bushes, clogging and trampling. The study is based on the results of expeditionary field research. A map of degradation centers of natural territorial complexes of the subalpine and alpine highlands of Chornohora in the vicinity of Brebeneskul Lake on a scale of 1 : 10 000 at the level of simple tracts and subtracts with the use of modern mapping methods is made. Peculiarities of formation, area and configuration, as well as landscape differentiation of centers of development of degradation processes of high-mountain landscape complexes in the vicinity of Brebeneskul Lake are analyzed. It is established that the most recreational load is experienced by the complex tract of my-boulder moraine-scree bottom of the Brebeneskul Cirque of the south-eastern exposition. The cutting of mountain pine (Pinus mugo Turra) and littering on the area of about 0,8 ha, trampling of the soil and vegetation cover on the area of 1,0 ha were recorded here. The deterioration of the ecological situation in the vicinity of Brebeneskul Lake is the result of unorganized recreational and tourist activities. Recommendations for reducing the negative impact of recreational activities and reducing the degradation of natural territorial complexes subalpine and alpine highlands of Chornohora in the vicinity of Brebeneskul Lake are outlined.


Author(s):  
Alexey Verkhoturov ◽  
Vyacheslav Melkiy

Explosive volcanic eruptions pose certain danger for natural environment, transport communications and other objects of human economic activity due to the fact that during such eruptions, up to several cubic kilometers of volcanic ash and aerosols can enter to atmosphere in long time. The research of extent of the impact of volcanic eruptions on surrounding area and the determination of their consequences contributes to reasonable assessment of volcanic hazard and possible risks in time conduct of economic activities and ensuring for safe location of settlements, enterprises, sea way and air lines. Chikurachki volcano is one from most active on territory of the Kuril Island Arc. In articles of volcanologists is information about eruptions in 1853–1859, 1958, 1961, 1964, 1973, 1986, 2002, 2003, 2005, 2007, 2008, 2015, 2016. The vegetation index (NDVI) used as means of assessing state of the natural environment. The boundary dividing areas with disturbed and healthy vegetation cover taken along isoline with NDVI value of 0.4. Schematic maps of the dynamics of boundary isolines according for the vegetation index from 1972 to 2020 has been compiled. The dynamics of vegetation cover in the north-eastern, south-eastern and southern sectors relative to Chikurachki volcano is revealed. The north-eastern sector experienced strong negative impact of eruption of the Chikurachki volcano in 1853, at later (2007 and 2015) only ash falls were observed in this direction. The vegetation cover outside the isoline NDVI = 0.4 has almost completely recovered to 2020. The south-eastern sector damaged during eruption of 1986, and was also subject for periodic tephra precipitation and ash falls during 2002–2016. Vegetation was completely destroyed at distance of 9 km from the crater of the volcano, and also valley forests on Tukharka River were destroyed. In southern sector in upper part of the Vernadsky Ridge, harsh growing conditions do not allow vegetation to recover for decades. At the same time, on eastern and western slopes of the ridge, after eruptions with deposition of tephra by layer of small thickness, alder elfin restoration few years. The results of the recearch can be used in forecasting volcanic hazards and rapid assessment of impact on natural environment of territories adjacent to volcanoes of this type as a result of volcanic eruptions.


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