Map of Indian Territory

Survey map of Indian Territory by the Department of the Interio

Map of Indian Territory

Map of Indian Territory showing the progress of sub-division surve

Compactación del suelo durante la cosecha forestal: evolución de las propiedades físicas Soil compaction by forestry harvester operation: evolution of physical properties

Se realizaron ensayos en campo con el objeto de evaluar los efectos y la persistencia de la compactación inducida por diferentes intensidades de tránsito durante la cosecha forestal en una población de álamos (Populus sp.). Se trabajó con un tractor de tracción simple de 73,5 kW y un acoplado, con una masa de 4,2 Mg y 2,7 Mg, respectivamente. Se establecieron 3 tratamientos de tránsito: 1, 5 y 10 pasajes sobre una misma senda, contrastados con un testigo sin tránsito. Luego de cada tratamiento, y 3 años después de realizados los mismos, se efectuaron determinaciones de penetrometría, densidad aparente y humedad gravimétrica. Hubo incrementos significativos de resistencia a la penetración para los tratamientos con tránsito, alcanzando el de mayor intensidad valores entre el 76 y el 16 % en los primeros 40 cm de profundidad. La densidad aparente tuvo una tendencia similar limitada a una menor profundidad. Luego de 3 años, los efectos persistían a nivel subsuperficial, para el índice de cono en los sectores tránsitados con respecto a los no transitados, encontrándose diferencias significativas para el tratamiento de 10 pasajes respecto al de 1 pasaje hasta 50 cm. Aún con cargas por eje de 3 Mg, el incremento de la intensidad de tránsito induce compactación a nivel subsuperficial que persiste en el tiempo.<br>The long-term effects on soil compaction by different traffic intensities during forestry harvester operation were evaluated in field experiments on heavy clay, vertic Argiudol. A conventional 2WD 73.5 kW engine power tractor with a trailer, 4.2 Mg and 3.75 Mg total load respectively, were used on a multiclonal Populus deltoides (Marsh) 3x3 plantation. There were four treatments: one pass, five pass and ten repeated passes with the tandem over the same track, and a control plot without experimental traffic. Moisture content, bulk density and penetrometer resistances were evaluated before and immediately after the traffic treatments and three years later. Effects of induced soil compaction by traffic were especially marked on topsoil, with cone index increments between 76 and 16% in the first 40 cm of the surface layer after treatments. Bulk density had a similar tendency but limited to a 15 cm depth. Three years later, only subsoil cone index in the track line, below 20 cm depth, was significantly higher than the interline track soil cone index. The 10 passes treatment had significant differences compared to the 1 pass and no traffic control plot treatments from the surface layer to 50 cm depth, without differences with the 5 passes treatment in most of the studied soil layers. Subsoil compaction may be induced by repeated traffic with low axle load and their effects persist for a very long time

The historical sociology of muslim societies: Khaldunian applications

10.1177/0268580907076570International Sociology223267-28

On the origin of A-tents (pop-ups), sheet structures, and associated forms

Copyright © 2009 by SAGE PublicationsA-tents are also known as pop-ups and by several other local names. They consist of raised slabs or plates of various thicknesses and origins. Laminae are caused by weathering, and spall plates or slabs may be caused in part by freeze-thaw acting on water held in pre-existing partings which are, however, like the sheet fractures that define the thicker sheet structures, probably of tectonic origin. A-tents are the result of the buckling of such laminae, plates and slabs. Again, tectonism in the form of compressive horizontal stress, appears the most likely and common causation, though decreases in lithostatic pressure consequent on unloading and, in particular cases, surficial expansion of plates caused by the intense heat of fires, may also contribute to rock failure and rupture. All A-tents are of Holocene age and are, therefore, neotectonic forms. Some have developed in living memory, and some are known to be developing from blisters. There is some evidence of continued dislocation along sheet fractures and of the transformation of blisters or arches into A-tents under the influence of continued lateral compression. This review demonstrates, therefore, that A-tents, sheet structures, and associated forms share a common heritage