Most Popular Books by Barbara Baker

Dream Gardens of England is a beautifully designed, inspirational sourcebook celebrating 100 gardens of all sizes and styles from across the country. From Yorkshire to Cornwall, and from Kent to Gloucestershire; from a tiny tropical paradise in the centre of Norwich to a large, spectacularly landscaped estate in the Gloucestershire countryside: the selection is wonderfully varied, and the skill and dedication of the designers and owners simply breathtaking. -- Jacket.

Do you feel you tried everything to make positive changes in your life with little success? Is the brokenness in you preventing you from moving forward in life? Are you ready to break the bondage of brokenness, rejection, and unforgiveness? In this book, you will discover how the power of the Holy Spirit can heal the wounded places of the heart. You will discover a fresh hope for a better life as you open yourself up to the remarkable and loving work of the Holy Spirit. This is your time!

Results of a survey of Alaskan commercial saltwater fisheries, giving statistics on employment, wages, and seafood processing.

A curriculum teaching children conflict solving skills.

Fog has been shown to be an important water source for coastal vegetation, but the extent to which fog influences soil processes and hydrology has not been well studied. Precipitation inputs from fog and rain, along with soil moisture and throughfall under Bishop pine (Pinus muricata) canopy, were measured at two site pairs on Santa Cruz Island, California. Fog drip is an integral part of the hydrologic cycle in the moisture-limited environments of Santa Cruz Island, and contributes moisture to the soil profile that is then available for plant uptake or soil decomposition and weathering processes while temperatures are highest. In a litterbag decomposition experiment performed over 3 years, decomposition rates of both pine and grass litter were highest at the pine sites, suggesting that moisture is a limiting factor in this environment. On a total profile basis, total pedogenic iron (Fed̳) and Feo̳/Fed̳ ratios also indicate that the pine soils are more weathered than the grass soils, and that the schist soils may be more weathered that the rhyolitic tuff/breccia soils. The apparent ratio of kaolinite to smectite, based on XRD peak intensity, is highest in the upper horizons and decreases with depth. Fog events occurred dominantly during summer months, and were generally enriched in isotope values compared to rain events, which occurred mainly during winter months. Isotope values of soil solution indicate that grass sites are influenced by evaporation, while pine canopy sites show minimal evaporation effects. The [delta]D values of the phyllosilicates range from -64.3 to -94.3, and [delta]18O values range from 19.8 to 25.1. The estimated temperatures of crystallization range from 7 to 22 °C, with grass sites showing a greater difference in temperature than pine sites between surface and subsurface horizons. It is possible that fog inputs contribute to the lower estimated surface temperatures of crystallization at the pine sites; however, estimates of meteoric water composition in equilibrium with phyllosilicates indicate consistently depleted surface water isotope values compared to subsurface values at all sites.