Assessment of ecological flexibility of winter rye varieties in the arid zone of the north of the Astrakhan region

Author(s):  
Valentina A. Fedorova ◽  
Author(s):  
А. B. Biarslanov ◽  
Z. G. Zalibekov ◽  
Z. U. Gasanova ◽  
P. А. Abdurashidova ◽  
V. А. Zhelnovakova ◽  
...  

The paper is devoted to soil cover degradation in the northen part of the Republic of Dagestan. Soil degradation is affected by irrational using free flowing underground water of artesians. Intensive extraction of underground water for domestic drinking water supply and pastures watering leads to irreversible processes in the soil cover. The study of salt spreading processes in soils caused by technogenic pressure is mainly considered for humid zone, in arid zone such work was not carried out. In this regard, the aim of the study is to clarify the state of the salt balance of soils for possible technogenic halogenesis under the conditions of a long half-century, continuous impact of artesian sources. The analysis of the territorial spreading of salts is considered on the example of soils of the marine coast and the central part of the Terek-Kuma lowland, represented by varieties of meadow saline and light chestnut soils. Taking into account the conditions of mutual location, experimental plots were selected with reference to artesian sources in the marine coast and in the continental part. Experimental and control sections were laid at experimental plots. Soil samples and artesian water samples were tested for the content of light soluble salts using conventional methods. It was established that under conditions of self-flowing artesian sources the soil of the continental part is characterized by an increased salt content and is 0.26-0.48% according to the profile against the background of the salt content in the samples of control plots – 0.11-0.17%. Coastal soils are characterized by a higher degree of salinization, the influence of mineralized water sources has a desalinization impact. On the test plot the salt content is 0.31–0.51%, in the control plot – 1.22–4.29%.


1988 ◽  
Vol 36 (4) ◽  
pp. 385 ◽  
Author(s):  
BR Maslin ◽  
L Pedley

Patterns of distribution are described for the three subgenera and nine sections that make up the Australian Acacia flora. Subgenus Phyllodineae (833 species) is widespread and contains 99% of the species; subgenus Acacia (six species) and subgenus Aculeiferum (one species) are poorly represented and virtually confined to the north of the continent. The geographic patterns of species-richness are strongly influenced by sections Phyllodineae (352 species), Juliflorae (219 species) and Plurinerves (178 species). Section Phyllodineae has centres of richness south of the Tropic of Capricorn in temperate and adjacent semiarid areas of eastern, south-eastern and south-western Australia. The section is poorly represented in the tropics. The closely related sections Juliflorae and Plurinerves predominate in the north of the continent, semiarid areas of the south-west, many rocky tablelands of the Arid Zone and along the Great Dividing Range and adjacent inland riverine lowland areas in eastern Australia. The remaining four sections contribute little to the overall patterns of species-richness. The principal speciespoor areas are sandy and fluvial lowland regions of the Arid Zone. In eastern Australia, sections Botrycephalae, Juliflorae, Phyllodineae and Plurinerves show discontinuous patterns of species-richness along the Great Dividing Range. All sections have species whose ranges terminate in the area of the McPherson-Macleay Overlap region.


1949 ◽  
Vol 21 (1) ◽  
pp. 125-142
Author(s):  
E. A. Jamalainen

In the middle and northern parts of Sweden and Finland Gramineae-planti are infected by a fungus of Sclerotinia-genus which causes injury during the overwintering of the plants. Vleugel in Sweden described the fungus with the name Sclerotinia borealis Bubåk and Vleugel in 1917. In Sweden S. borealis has been met in several years causing injury to winter rye, timothy, cocksfoot and other field grasses. It occurs commonly in Norrland, especially in the country Norrbotten. The southern limit of its spreading area in Sweden is in latitude about 61° N. In Finland S. borealis is met in the middle and northern parts of the country. On the basis of the information hitherto the fungus is more or less general in the years favourable to its occurrence in the provinces of Lapland, Oulu, Kuopio and Mikkeli. When occurring more abundantly as happened during the overwintering 1945—46, S. borealis is in these regions one cause for the poor overwintering of winter rye, timothy and other grasses. The climatical conditions prevailing during autumn, winter and spring are of decisive bearing for the spreading of S. borealis as well as for its abundant occurrence in certain years. The development of the apothecia of the fungus and the spreading of the ascospores is evidently favoured by long, rainy autumn, the damages are promoted by low freezing of the soil and thick cover of snow in the winter as well as by slow melting of snow in the spring. Of the occurrence of S. borealis in different Gramineae-plants, see p. 133—134. Different varieties of winter cereals and species and strains of grasses vary greatly in resistance to S. borealis. It has been observed that, of the varieties of winter rye, especially the Finnish ones resist the disease caused by the fungus very well. Of field grasses, Phleum pratense, Dactylis glomerata, Lolhim perenne, Poa serotina, and P. trivialis are susceptible to S. borealis. Some strains of these species, however, are extremely well resistant to the fungus. The strains of the grasses and varieties of winter rye grown in the north are generally more resistant to the damages by the fungus. In developing new varieties of winter cereals and strains of field grasses for the northern conditions these facts must be duly considered and for the breeding work such material should be selected which has grown in the district where the fungus occurs. Obviously the damages caused by the fungus are less when the plants receive plenty of nutrients, especially phosphates whereby they become stronger to resist infections.


Author(s):  
Ahmed Abubakar Jajere ◽  
Adam Modu Abbas ◽  
Ali Abdu

This study used annual rainfall records from three stations within the North East Arid Zone of Nigeria for the period (1957-2017) to measure the extent of the rainfall recovery by comparing the drought decades and post drought decades rainfall patterns. Monthly rainfall records from Potiskum, Maiduguri and Nguru Stations were used. Descriptive and inferential statistical tools were employed in analysing the data. The findings of the study revealed a significant year-to-year variability in rainfall characteristics around 61 years (1957-2017) averages. The variability was large in 1970s up till 1990s, and lower in 1960s and from 2000 to 2018. Decreasing trend in annual rainfall amount was observed during the study period while a stability in onset and cessation dates were observed. The differences between 1957-1986 and 1987-2017 climatic season were found to be statistically insignificant. The study concluded that the reported rainfall recovery from drought is statistically insignificant and the observed long term mean trend revealed a decreasing trend. Therefore, the theory of Sahel rainfall recovery can be better termed as a ‘’break of the series of drought or decline in frequency and magnitude of occurrence of drought’’ The research recommended the continuations with the drought adaptation and mitigation strategies adopted by local population, decisions makers and organizations following the series Sahelian droughts of 1970s and 1980s.


2021 ◽  
pp. 21-46
Author(s):  
Jagjeet Lally

This chapter introduces the structure and organisation of caravan trade. Focusing on the environment, it opens by connecting the wave of political flux and state-building to the shock of the Little Ice Age, which hit Afro-Eurasia around the mid-seventeenth century. It then sketches the broad geography and circulatory pattern along the north-south routes from the Eurasian interior to the Indian subcontinent. It shows that exchange was based on specialisation and interdependence between the arid zone that stretched from central Asia to the Indo-Afghan frontier and the wet zone of monsoon south Asia, and was subject to seasonal rhythms, with climate shaping when—and through which routes—it was hospitable to pass. It also demonstrates that ecological change—as well as economic and political factors—could shift patterns of specialisation and thereby affect trade, illustrated through a case study of the Indo-central Asian horse trade.


Water ◽  
2019 ◽  
Vol 11 (1) ◽  
pp. 84 ◽  
Author(s):  
Ashraf M. Mushtaha ◽  
Marc Van Camp ◽  
Kristine Walraevens

The Gaza Strip forms a transition zone between the semi-humid coastal zone in the north, the semi-arid zone in the east, and the Sinai desert in the south. Groundwater is the only water source for 1.94 million inhabitants, where the only fresh replenishment water for the aquifer comes from rainfall. This study focuses on testing a newly developed GIS tool to estimate the spatial and temporal distribution of runoff and recharge from rainfall. The estimation of surface runoff was made using the Soil Conservation Services Curve Number Method, while groundwater recharge was estimated using Thornthwaite and Mather’s Soil Moisture Balance approach. The new tool was applied to the Gaza aquifer for the year 1935 and for the period from 1973 to 2016. A comparison was made between the results obtained with the developed GIS tool and the frequently used Thiessen polygon method for rainfall distribution. Runoff and recharge were estimated for the year 1935 (prior to development) to compare with the current developed conditions. It was found that the built-up and sand dune areas stand in an inverse relationship, where the former is replacing the latter (built-up area expanded from 30.1 km2 in 1982 to 92.1 km2 in 2010). Recharge takes place in the sand dune area, whereas runoff increases in the built-up area. Due to development, runoff almost tripled from 9 million m3 in 1982 to 22.9 million m3 in 2010, while groundwater recharge was reduced from 27.3 million m3 in 1982 to 23 million m3 in 2010, even though the rainfall increased between 1982 and 2010 by 11%. Comparison between the newly developed GIS tool and the Thiessen polygon-based estimation shows that the former leads to higher values of runoff and recharge for dry years.


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