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481.
The change of the Maasai from pure pastoralists to agropastoralists has brought about serious problems for them. This paper tries to analyse this process of change and to throw some light on the resultant problems. First, it is being shown how the climate of the Maasai Steppe is too dry for a successful cultivation of maize by them, which has become their main food. Successive crop failures and high labour costs have rendered maize-growing a losing-business for the Maasai. Moreover, the State policy of granting certificates of occupancy in the Maasai land to outsiders allowing them to make large-mechanized farms, has alarmed the Maasai so much that many of them rushed back to their home areas to rescue their land from being grapped by other ethnic groups. Thus, they began to abandon their traditional grazing-movements, which are highly adapted to the ecological conditions of the Maasai Steppe. At the same time, the herds of the Maasai were decimated, because of the spread of animal diseases following the deterioration of the State veterinary service system. Added to this are the losses incurred through distress sales of cattle for buying maize for food, at a time at which the maize prices are increasing at a much higher rate than the prices of livestock. This dilemma of the Maasai and their indigenous coping mechanisms are being illustrated by the case of the people of Mokia at Namalulu, with special consideration of the role of women in solving these problems. 相似文献
482.
483.
Specific electrical conductivity (SEC), total dissolved solids (TDS), and silica (SiO2) are ground-water quality parameters routinely measured in a laboratory. Electrical conductivity measurements are made quickly and are less costly than TDS measurements. Once the relationship between the parameters is determined by regression analysis, TDS can be estimated quickly from the SEC and SiO2 measurements. Water quality data from 25 city wells in Fresno, California, and historical ground-water quality data from the adjacent San Joaquin River/Kings River alluvial interfan (central San Joaquin Valley, California), the Kaweah River alluvial fan, and the Kern River alluvial fan (southern San Joaquin Valley) were used in this investigation. For the specific hydrologic areas studied, the model's TDS predictive ability is improved when SiO2 is included with SEC as the independent variables. 相似文献
484.
Barbara Obrebska-Starkel 《GeoJournal》1984,8(3):259-263
In the Polish Carpathian Mountains two altitudinal profiles were chosen. Ranging from 200 to 1,000 m asl along 20°00 and 21°30E their spatial patterns of the topographical types in the mountains and uplands, geometric configuration of concave topographies and direction of their course are different.The effects of topography on the mesoclimatic conditions in the area investigated were analyzed by the diurnal air temperature records at the 28 meteorological stations in the years 1951 – 1970. Along the two profiles, taking the points situated at the same height asl and similar altitude, the mean extreme temperatures in the particular months, as well as the values of the first and ninth deciles of the maximum and minimum temperatures were analyzed. Special consideration was given to the spatial distribution of the minimum temperature and characteristics derived, because it reflects the influence of topography in a higher degree than the maximum temperature. Since low air temperatures are the main factor for the plant growth in the Polish Carpathians, spatial differentiation of the minimum temperature regulates the rate of development of the wild and cultivated plants during the growing season. 相似文献
485.
Barbara Hennemuth 《Boundary-Layer Meteorology》1986,36(4):371-394
Wind observations from a small Alpine valley are used to investigate the problem of cross-valley winds. The observed daytime windfield is a superposition of dynamically and thermally forced cross-winds. Prevailing cross-winds above the valley result in a recirculation cell above the lee slope. The return flow is strengthened or weakened by thermal effects which induce a wind that blows from the shaded to the sunny side of the valley. The reaction time of the thermally induced cross-winds is only 4 min. The horizontal and vertical motions of the cross-valley circulation transport heat in such a way that the insolation differences between the two sides of the valley are nearly equalized. 相似文献
486.
Couplings of watersheds and coastal waters: Sources and consequences of nutrient enrichment in Waquoit Bay,Massachusetts 总被引:1,自引:0,他引:1
Ivan Valiela Kenneth Foreman Michael LaMontagne Douglas Hersh Joseph Costa Paulette Peckol Barbara DeMeo-Andreson Charlene D’Avanzo Michele Babione Chi-Ho Sham John Brawley Kate Lajtha 《Estuaries and Coasts》1992,15(4):443-457
Human activities on coastal watersheds provide the major sources of nutrients entering shallow coastal ecosystems. Nutrient loadings from watersheds are the most widespread factor that alters structure and function of receiving aquatic ecosystems. To investigate this coupling of land to marine systems, we are studying a series of subwatersheds of Waquoit Bay that differ in degree of urbanization and hence are exposed to widely different nutrient loading rates. The subwatersheds differ in the number of septic tanks and the relative acreage of forests. In the area of our study, groundwater is the major mechanism that transports nutrients to coastal waters. Although there is some attenuation of nutrient concentrations within the aquifer or at the sediment-water interface, in urbanized areas there are significant increases in the nutrient content of groundwater arriving at the shore’s edge. The groundwater seeps or flows through the sediment-water boundary, and sufficient groundwater-borne nutrients (nitrogen in particular) traverse the sediment-water boundary to cause significant changes in the aquatic ecosystem. These loading-dependent alterations include increased nutrients in water, greater primary production by phytoplankton, and increased macroaglal biomass and growth (mediated by a suite of physiological responses to abundance of nutrients). The increased macroalgal biomass dominates the bay ecosystem through second- or third-order effects such as alterations of nutrient status of water columns and increasing frequency of anoxic events. The increases in seaweeds have decreased the areas covered by eelgrass habitats. The change in habitat type, plus the increased frequency of anoxic events, change the composition of the benthic fauna. The data make evident the importance of bottom-up control in shallow coastal food webs. The coupling of land to sea by groundwater-borne nutrient transport is mediated by a complex series of steps; the cascade of processes make it unlikely to find a one-to-one relation between land use and conditions in the aquatic ecosystem. Study of the process and synthesis by appropriate models may provide a way to deal with the complexities of the coupling. 相似文献
487.
Barbara J. Leitner Donald J. Weidner Robert C. Liebermann 《Physics of the Earth and Planetary Interiors》1980,22(2):111-121
The elastic moduli of a synthetic single crystal of pyrope (Mg3Al2Si3O12) have been determined using a technique based on Brillouin scattering. These results are used in an evaluation of the effect of composition on the elastic properties of silicate garnet solid solution series (Mg, Fe, Mn, Ca)3 (Al, Fe, Cr)2 Si3O12. In the pyralspites (Mg FeMn aluminum garnets), for which a large amount of data is available, this analysis indicates that the bulk modulus K is independent of the Fe2+/Mg2+ ratio, which is similar to the behavior observed in olivines and pyroxenes. However, the shear modulus μ of the garnets increases by 10% from the Mg to the Fe end member, in contrast to the decrease of μ with Fe content which is observed in olivines and pyroxenes. This contrasting behavior is most probably related to the oxygen coordination of the cation site occupied by Mg2+ and Fe2+ in these different minerals. 相似文献
488.
489.
Dynamic capillary effects in heterogeneous porous media 总被引:1,自引:0,他引:1
In standard multi-phase flow models on porous media, a capillary pressure saturation relationship developed under static conditions
is assumed. Recent experiments have shown that this static relationship cannot explain dynamic effects as seen for example
in outflow experiments. In this paper, we use a static capillary pressure model and a dynamic capillary pressure model based
on the concept of Hassanizadeh and Gray and examine the behavior with respect to material interfaces. We introduce a new numerical
scheme for the one-dimensional case using a Lagrange multiplier approach and develop a suitable interface condition. The behavior
at the interface is discussed and verified by various numerical simulations. 相似文献
490.
K. David Newell John H. Doveton Daniel F. Merriam Barbara Sherwood Lollar William M. Waggoner L. Michael Magnuson 《Natural Resources Research》2007,16(3):277-292
In late 2005 and early 2006, the WTW Operating, LLC (W.T.W. Oil Co., Inc.) #1 Wilson well (T.D. = 5772 ft; 1759.3 m) was drilled
for 1826 ft (556.6 m) into Precambrian basement underlying the Forest City Basin in northeastern Kansas. Approximately 4500
of the 380,000 wells drilled in Kansas penetrate Precambrian basement. Except for two previous wells drilled into the arkoses
and basalts of the 1.1-Ga Midcontinent Rift and another well drilled in 1929 in basement on the Nemaha Uplift east of the
Midcontinent Rift, this well represents the deepest penetration into basement rocks in the state to date. Granite is the typical
lithology observed in wells that penetrate the Precambrian in the northern Midcontinent. Although no cores were taken to definitively
identify lithologies, well cuttings and petrophysical logs indicate that this well encountered basement metamorphic rocks
consisting of schist, gneiss, and amphibolitic gneiss, all cut by aplite dikes.
The well was cased and perforated in the Precambrian, and then acidized. After several days of swabbing operations, the well
produced shows of low-Btu gas, dominated by the non-flammable component gases of nitrogen (20%), carbon dioxide (43%), and
helium (1%). Combustible components include methane (26%), hydrogen (10%), and higher molecular-weight hydrocarbons (1%).
Although Coveney and others [Am. Assoc. Petroleum Geologists Bull., v. 71, no, 1, p. 39–48, 1987] identified H2-rich gas in two wells located close to the Midcontinent Rift in eastern Kansas, this study indicates that high levels of
H2 may be a more widespread phenomenon than previously thought. Unlike previous results, the gases in this study have a significant
component of hydrocarbon gas, as well as H2, N2, and CO2. Although redox reactions between iron-bearing minerals and groundwater are a possible source of H2 in the Precambrian basement rocks, the hydrocarbon gas does not exhibit the characteristics typically associated with proposed
abiogenic hydrocarbon gases from Precambrian Shield sites in Canada, Finland, and South Africa. Compositional and isotopic
signatures for gas from the #1 Wilson well are consistent with a predominantly thermogenic origin, with possible mixing with
a component of microbial gas. Given the geologic history of uplift and rifting this region, and the major fracture systems
present in the basement, this hydrocarbon gas likely migrated from source rocks and reservoirs in the overlying Paleozoic
sediments and is not evidence for abiogenic hydrocarbons generated in situ in the Precambrian basement. 相似文献