E M White
Biographic Data
| ID | 3975641 |
|---|---|
| NAME | E M White |
| GIVEN NAMES | E M |
| FAMILY NAME | White |
| SIGNATURE | WHITE E M |
| AFFILIATIONS | South Dakota State University |
| VERIFIED | No |
| TOTAL WORKS | 6 |
| TOTAL CITATIONS | 21 |
| AUTHOR COUNT | 6 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1928 |
| LATEST PUBLICATION YEAR | 1998 |
| H-INDEX | 1 |
Soil Changes beneath Stones in Mosaics and Tipi Rings
The weight of a stone placed on the soil surface will compact the underlying soil. The boundary between noncalcareous surface soil and underlying calcareous soil will appear to move downward in comparison to the noncompacted adjacent soils. Changes below the stone, other than compaction, would be difficult to measure and interpret
Cross sectional stature and weight reference curves for the UK, 1990.
The current reference curves of stature and weight for the UK were first published in 1966 and have been used ever since despite increasing concern that they may not adequately describe the growth of present day British children. Using current data from seven sources new reference curves have been estimated from birth to 20 years for children in 1990. The great majority of the data are nationally representative. The analysis used Cole's LMS metho…
Chemical Weathering of Bone in Archaeological Soils
Weathering of hydroxyapatite, Ca5(PO4)3(OH) in bone probably is initiated by organic and carbonic acids formed by the microbial decomposition of collagen. This weathering, independent of soil properties, is caused by protons replacing Ca from hydroxyapatite. As collagen is depleted, proton production decreases and weathering may either continue if protons are available from the soil or be arrested if Ca from the soil displaces the protons previou…
Cautionary Note on Soil Phosphate Data Interpretation for Archaeology
Data reporting the relative amounts of PO4 in different forms will have limited value for archaeology if data for the undisturbed soil are not available
Recent Gully Formation In Prairie Areas Of The Northern. Great Plains
Modern gully formation in the Great Plains and Southwestern United States has been attributed variously to overgrazing, farming, and climatic change. Pre-settlement prairie fires in the Northern Great Plains burned the protective vegetation so that gradients of drainageways were adjusted to more sediment than they receive today when wild fires are uncommon. Gully cutting may be an adjustment of the gradient to new conditions. Erosion caused by ov…
The Girl Voter
Chemical Weathering of Bone in Archaeological Soils
Weathering of hydroxyapatite, Ca5(PO4)3(OH) in bone probably is initiated by organic and carbonic acids formed by the microbial decomposition of collagen. This weathering, independent of soil properties, is caused by protons replacing Ca from hydroxyapatite. As collagen is depleted, proton production decreases and weathering may either continue if protons are available from the soil or be arrested if Ca from the soil displaces the protons previou…
Cautionary Note on Soil Phosphate Data Interpretation for Archaeology
Data reporting the relative amounts of PO4 in different forms will have limited value for archaeology if data for the undisturbed soil are not available
The Girl Voter
Recent Gully Formation In Prairie Areas Of The Northern. Great Plains
Modern gully formation in the Great Plains and Southwestern United States has been attributed variously to overgrazing, farming, and climatic change. Pre-settlement prairie fires in the Northern Great Plains burned the protective vegetation so that gradients of drainageways were adjusted to more sediment than they receive today when wild fires are uncommon. Gully cutting may be an adjustment of the gradient to new conditions. Erosion caused by ov…
Cautionary Note on Soil Phosphate Data Interpretation for Archaeology
Data reporting the relative amounts of PO4 in different forms will have limited value for archaeology if data for the undisturbed soil are not available
Chemical Weathering of Bone in Archaeological Soils
Weathering of hydroxyapatite, Ca5(PO4)3(OH) in bone probably is initiated by organic and carbonic acids formed by the microbial decomposition of collagen. This weathering, independent of soil properties, is caused by protons replacing Ca from hydroxyapatite. As collagen is depleted, proton production decreases and weathering may either continue if protons are available from the soil or be arrested if Ca from the soil displaces the protons previou…
Cross sectional stature and weight reference curves for the UK, 1990.
The current reference curves of stature and weight for the UK were first published in 1966 and have been used ever since despite increasing concern that they may not adequately describe the growth of present day British children. Using current data from seven sources new reference curves have been estimated from birth to 20 years for children in 1990. The great majority of the data are nationally representative. The analysis used Cole's LMS metho…
Soil Changes beneath Stones in Mosaics and Tipi Rings
The weight of a stone placed on the soil surface will compact the underlying soil. The boundary between noncalcareous surface soil and underlying calcareous soil will appear to move downward in comparison to the noncompacted adjacent soils. Changes below the stone, other than compaction, would be difficult to measure and interpret
Geology (4 works) · Geology (4 works) · Archaeology (2 works) · Geography (2 works) · Soil Science (2 works) · Soil Science (2 works) · Soil water (2 works) · Aeolian processes and effects (1 works) · Agriculture (1 works) · Archaeology and ancient environmental studies (1 works)