Forest Succession on the Republican River Floodplain in Clay County, Kansas

1974 ◽  
Vol 19 (2) ◽  
pp. 155 ◽  
Author(s):  
R. Glenn Bellah ◽  
Lloyd C. Hulbert
Keyword(s):  
Forest Succession ◽  
River Floodplain ◽  
Republican River

Spatially explicit modelling of floodplain forest succession: interactions among flood inundation, forest successional processes, and other disturbances in the Upper Mississippi River floodplain, USA

2019 ◽  
Vol 405 ◽  
pp. 15-32 ◽  
Author(s):  
Nathan R. De Jager ◽  
Molly Van Appledorn ◽  
Timothy J. Fox ◽  
Jason J. Rohweder ◽  
Lyle J. Guyon ◽  
...  
Keyword(s):  
Mississippi River ◽  
Forest Succession ◽  
Floodplain Forest ◽  
Spatially Explicit ◽  
Flood Inundation ◽  
Upper Mississippi River ◽  
River Floodplain ◽  
Inundation Forest

Erratum: Soil solution chemistry in relation to forest succession on the Tanana River floodplain, interior Alaska

2007 ◽  
Vol 37 (8) ◽  
pp. 1523-1523
Author(s):  
John Yarie ◽  
Keith Van Cleve ◽  
C. T. Dyrness ◽  
Lola Oliver ◽  
Jim Levison ◽  
...  
Keyword(s):  
Soil Solution ◽  
Forest Succession ◽  
Solution Chemistry ◽  
Soil Solution Chemistry ◽  
River Floodplain ◽  
Interior Alaska

Patterns of forest succession and impacts of flood in the Upper Mississippi River floodplain ecosystem

2009 ◽  
Vol 6 (4) ◽  
pp. 463-472 ◽  
Author(s):  
Yao Yin ◽  
Yegang Wu ◽  
Steve M. Bartell ◽  
Robert Cosgriff
Keyword(s):  
Mississippi River ◽  
Forest Succession ◽  
Upper Mississippi River ◽  
River Floodplain

Soil-solution chemistry in relation to forest succession on the Tanana River floodplain, interior Alaska

1993 ◽  
Vol 23 (5) ◽  
pp. 928-940 ◽  
Author(s):  
John Yarie ◽  
Keith Van Cleve ◽  
C.T. Dyrness ◽  
Lola Oliver ◽  
Jim Levison ◽  
...  
Keyword(s):  
River Water ◽  
Soil Solution ◽  
Forest Succession ◽  
Soil Surface ◽  
Solution Chemistry ◽  
Soil Solution Chemistry ◽  
River Floodplain ◽  
Interior Alaska ◽  
At Iii ◽  
Successional Stages

The chemical composition of soil solution reflects the demand of soil biological processes and the solubility and ion-exchange equilibria between physical and biological components of the soil. The objectives of this study were to document soil-solution chemistry for representative phases of the primary successional sequence on the Tanana River floodplain near Fairbanks, Alaska, and to assess the effect of physical versus biological control on solution chemistry in these sites. Soil-solution samples were collected weekly using porous-cup soil-solution samplers located 20, 50, and 150 cm below the soil surface. In addition, groundwater and river water samples were collected at several sites that represented the successional stages typical of the Tanana River floodplain of interior Alaska. Magnesium, HCO3, Cl, Na, K, NO3, and PO4 showed the highest concentrations in the 50-cm layer at each site. Manganese, Fe, and Zn showed the highest concentrations at the groundwater level. Aluminum and Ca showed decreasing concentrations with depth from the surface. Silicon displayed no specific depth trends. Ammonium was the only ion that was more concentrated in river water than in soil solution. Soil-solution pH showed no specific depth trends. Conductivity of the soil solution was generally lower at greater depths and was much lower in the river water. Sulfate, K, Ca, and Mn decreased in concentration from the early successional stages to the later successional stages, although some year to year variability did occur. All measured concentrations except Zn displayed at least one significant change in concentration due to vegetation clearing. These differences can be summarized broadly as effects on nonbiologically cycled nutrients in the open willow stage (III) and changes in the biological cycling of nutrients in the poplar–alder and mature white spruce stages (V and VIII, respectively). Significant increases in concentration of Fe and Mn were found at III-B-T (stage III–site B–treated (i.e., cleared) plot) while Na, Mn, Fe, Ca, Mg, Si, and SO4 increased at III-A-T. At V-A-T significant increases were found in concentrations of NH4, NO3, PO4, SO4, K, Na, Ca, Mg, Mn, Fe, Al, Si, HCO3, and conductivity in 987. These same trends were repeated in 1988 with the exception of NO3, Fe, and Si, which showed no significant differences. As a result of clearing both V-A-T and V-B-T, Fe and Si significantly decreased in concentration at 50 cm, which was the opposite trend found at 150 cm. The Cl concentration at 50 cm decreased at V-A-T in 1987 but increased in 1988 as a result of clearing. V-B-T showed no effect of clearing in 1988 and only NO3, SO4, Ca, Mg, and conductivity increased in 1987. Chloride, Al, and Si decreased in concentration as a result of clearing in 1987 at V-B-T. Nitrate, NH4, Cl, and pH increased, while PO4, K, Na, Ca, Mg, Si, HCO3, and conductivity decreased, as a result of clearing in VIII-A-T. At VIII-B-T, NO3, K, Ca, Mg, Cl, HCO3, and conductivity increased as a result of clearing in 1987, while only NO3 increased in 1988. Bicarbonate, Cl, and pH showed significant decreases in 1987 and 1988 at VIII-B-T. The results of this study, combined with the results of other studies of these salt-affected floodplain soils, detailing the soil environment and control of evaporative movement of water to the soil surface support the hypotheses that: (i) the genesis and maintenance of surface salt crusts are controlled by the soil physical and chemical environments encountered on early-successional mineral soils and (ii) the disappearance of salt crusts and reduction in mineral soil salt concentrations are controlled by forest succession, which mediates the changing soil physical, chemical, and biological environment.

A spatial simulation model for forest succession in the Upper Mississippi River floodplain

2009 ◽  
Vol 6 (4) ◽  
pp. 494-502 ◽  
Author(s):  
Yao Yin ◽  
Yegang Wu ◽  
Steven M. Bartell
Keyword(s):  
Simulation Model ◽  
Mississippi River ◽  
Forest Succession ◽  
Upper Mississippi River ◽  
Spatial Simulation ◽  
River Floodplain ◽  
Spatial Simulation Model

Forest Succession and Sedimentation on a Meandering-River Floodplain, Northeast British Columbia, Canada

1977 ◽  
Vol 4 (3) ◽  
pp. 229 ◽  
Author(s):  
Gerald C. Nanson ◽  
Harry F. Beach
Keyword(s):  
British Columbia ◽  
Forest Succession ◽  
River Floodplain ◽  
Meandering River

Орошение томата F1 Донской в открытом грунте Московской области

2019 ◽  
Author(s):  
D.I. Engalychev ◽  
N.A. Engalycheva ◽  
A.M. Menshikh
Keyword(s):  
Experimental Data ◽  
Agricultural Technology ◽  
Tomato Fruits ◽  
River Floodplain ◽  
Yield And Quality ◽  
Open Ground ◽  
Alluvial Meadow ◽  
Standard Production ◽  
Moscow River

Представлены экспериментальные данные о влиянии капельного орошения на урожайность и качество плодов томата при выращивании культуры в открытом грунте Московской области. На плодородных аллювиальных луговых почвах Москворецкой поймы при соблюдении агротехники без орошения в среднем за три года исследований в полевых условиях получена урожайность томата F1 Донской 31,9 т/га, с орошением 48,5 т/га, в т.ч. стандартной продукции 42,6 т/га.The article presents experimental data on the effect of drip irrigation on the yield and quality of tomato fruits when growing crops in open ground of the Moscow Region. On fertile alluvial meadow soils of the Moscow river floodplain, with the observance of agricultural technology without irrigation, the field yield of tomato hybrid F1 Donskoi on average for three years of research was 31.9 t/ha, with irrigation 48.5 t/ha, incl. standard production 42.6 t/ha.

ASPECTS OF INVASIVE PLANTS DOMINATED HABITATS USE BY MARSH WARBLER (ACROCEPHALUS PALUSTRIS) IN SOMEȘ RIVER FLOODPLAIN

2018 ◽  
Vol 13 (2) ◽  
pp. 515-521
Author(s):  
Alexandru LAPOSI ◽  
◽  
Aurel ARDELEAN ◽  
Monica MARIAN
Keyword(s):  
Invasive Plants ◽  
River Floodplain ◽  
Marsh Warbler ◽  
Acrocephalus Palustris

Forest succession and earthworms composition in the Brazilian eastern amazon.

2017 ◽  
Author(s):  
Luis Manuel Hernandez GARCIA ◽  
sandriel costa SOUSA ◽  
Jesus Enrique Burgos GERRERO ◽  
Guillaume Xavier ROUSSEAU
Keyword(s):  
Forest Succession

On syntaxonomy of floodplain forests (Salicetea purpureae Moor 1958) of the Irtysh and Black Irtysh rivers

2005 ◽  
pp. 82-92
Author(s):  
G. S. Taran
Keyword(s):  
Populus Alba ◽  
Floodplain Forests ◽  
White Poplar ◽  
Salix Alba ◽  
River Floodplain ◽  
White Willow ◽  
Irtysh River

The paper characterizes poplar (Populus alba, P. nig­ra) and white willow (Salix alba) forests of the Irtysh and the Black Irtysh river floodplain, together with the silvery salt tree (Halimodendron halodendron) community of the Black Irtysh river floodplain. The Black Irtysh floodplain willow and poplar forests are separated into a new alliance, Rubio dolichophyllae—Populion albae Taran all. nov. (Salicetalia purpureae Moor 1958, Salicetea purpureae Moor 1958), which includes the associations Rubio dolichophyllae—Popu­letum albae Taran 1997 and Rubio dolichophyllae—Salicetum albae Taran ass. nov. The Halimodendron halodendron community is probably related to the class Nerio-Tamaricetea Br.-Bl. et de Bolós 1958. White poplar forests in the Irtysh R. upper reaches, described within the Semipalatinsk city limits, belong to the association Heracleo dissecti—Populetum albae Taran 1997 and its subassociation H. d. —P. a. lamietosum albi Taran 1997 (Equiseto hyemalis—Populion nigrae Taran 1997, Salicetalia purpureae Moor 1958).

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