chlorophyll-a and potassium-phosphate

Biological soil crusts (BSCs) cover >35% of the Earth's land area and contribute to important ecological functions in arid and semiarid ecosystems, including erosion reduction, hydrological cycling, and nutrient cycling. Artificial rapid cultivation of BSCs can provide a novel alternative to traditional biological methods for controlling soil and water loss such as the planting of trees, shrubs, and grasses. At present, little is known regarding the cultivation of BSCs in the field due to lack of knowledge regarding the influencing factors that control BSCs growth. Thus, we determined the effects of various environmental factors (shade; watering; N, P, K, and Ca concentrations) on the growth of cyanobacteria-dominated BSCs from the Sonoran Desert in the southwestern United States. The soil surface changes and chlorophyll a concentrations were used as proxies of BSC growth and development. After 4 months, five factors were found to impact BSC growth with the following order of importance: NH4NO3 ≈ watering frequency>shading>CaCO3 ≈ KH2PO4. The soil water content was the primary positive factor affecting BSC growth, and BSCs that were watered every 5 days harbored greater biomass than those watered every 10 days. Groups that received NH4NO3 consistently exhibited poor growth, suggesting that fixed N amendment may suppress BSC growth. The effect of shading on the BSC biomass was inconsistent and depended on many factors including the soil water content and availability of nutrients. KH2PO4 and CaCO3 had nonsignificant effects on BSC growth. Collectively, our results indicate that the rapid restoration of BSCs can be controlled and realized by artificial "broadcasting" cultivation through the optimization of environmental factors.

Topics: Biomass; Calcium Carbonate; Chlorophyll; Chlorophyll A; Cyanobacteria; Desert Climate; Ecology; Ecosystem; Lichens; Light; Nitrates; Phosphates; Poaceae; Potassium Compounds; Soil Microbiology; Southwestern United States; Temperature; Trees; Water

We investigated the interaction between trehalose and alkaline-earth metal ions. The nuclear relaxation times of carbon atoms of trehalose were shortened by addition of the alkaline-earth chloride salts, MgCl2, CaCl2, and SrCl2, indicating that trehalose formed metal-complexes with the alkaline-earth metal chlorides. From the data of the 1H-1H coupling constants of trehalose in the presence of the alkaline-earth chlorides, it appeared that trehalose formed complexes with MgCl2, and CaCl2 at the various complexing sites: Mg2+ was coordinated to O-4 and O-4' of trehalose, and Ca2+ to O-2 and O-3. We succeeded in the preparation of two types of crystals of the trehalose/CaCl2. One was a crystal consisting of trehalose, CaCl2, and water in a ratio of 1:1:1. The other was an anhydrous crystal containing trehalose and CaCl2 in a ratio of 1:2. Several applications of the complexing between trehalose and the metal ions for food processing are proposed.

Topics: Animals; Calcium Chloride; Carbohydrates; Chlorophyll; Crystallization; Magnesium Chloride; Meat; Molecular Conformation; Phosphates; Plant Leaves; Potassium Compounds; Spinacia oleracea; Strontium; Swine; Trehalose