Beauty for Ashes (A Hickory Ridge Romance, Book 2) by Dorothy Love

By Dorothy Love

She’s a stunning younger widow. He’s a Southern gentleman with a thirst for event. either want a position to name home.

After wasting her husband within the Civil warfare, Carrie Daly is scared she is going to by no means have the relatives she longs for. Eligible bachelors are scarce in Hickory Ridge, Tennessee, yet Carrie has came upon love. no longer the weak-in-the-knees sort, yet anything useful. nonetheless, she isn't relatively able to set a marriage date with Nate Chastain.

Griff Rutledge is a former member of Charleston society, yet has been estranged from his kinfolk for years. He’s made up our minds to stay unattached, by no means settling in a single position for too lengthy. but if requested to coach a Thoroughbred for an upcoming race in Hickory Ridge, he makes a decision to stick awhile.

Despite objections from the townsfolk, and her worry that real happiness has eluded her, Carrie is interested in Griff's kindness and grace. it's going to take a bounce of religion for them to open their hearts and declare God's promise to provide attractiveness for ashes.

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Additional info for Beauty for Ashes (A Hickory Ridge Romance, Book 2)

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E. Fogg, Arch. , Ergeb. , 1971, 5 , 1. 1° It was found that the concentration of extracellular compounds in a bacteria-free culture was greatly reduced in the presence of a mixed population of bacteria isolated from the lake in which these acids were found. Other extracellular algal products whose occurrence in natural waters has been discussed are polysaccharides, amino-acids, and polypeptides. 24 Studies on the secretion of dissolved material by macrophytes have shown that the littoral flora is a potential major source of dissolved organic matter (DOM) in lakes.

Wellman, and H. R. Krouse, International Symposium on Hydrogeochemistry and Biogeochemistry, Tokyo, September, 1970. 075 may be expected when cleavage of the N-0 bond is totally rate-controlling. g. 0%,,s7the total evidence strongly indicates that, in general, biologically combined nitrogen is enriched in 15N relative to the atmosphere, exceptions being legumes, which are capable of fixing atmospheric nitrogen directly. From this, Parker2' contends that denitrification processes, with the accompanying release of 'light' nitrogen into the atmosphere and the retention of 15N-enriched nitrate in the soil for subsequent biological utilization, probably largely control isotopic distribution.

1972,18,162. R. G. Wetzel and B. A. Manny, Limltol. , 1972, 17, 927. ), using a mixed culture obtained from a lake sediment, thus simulating decomposition at the sediment surface, has been studied under aerobic28and anaerobicz9conditions. Under aerobic conditionsthe production of dissolved organic matter was about 7 % as carbon and 6 % as nitrogen after 30 days, and a proteinaceous compound, giving 14 amino-acids on hydrolysis, was recognized in the dissolved fraction. The decomposition rate during this time followed approximate first-order kinetics, and the decomposition pattern of the cell nitrogen suggested that the algal residue could be divided into labile and refractory constituents according to their resistance to bacterial attack.

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