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Calcium makes up roughly 34% of the Earth s crust and has been around since the formation of the Earth It is found in igneous rocks as calcium silicates, and in sedimentary and metamorphic rocks as calcium carbonates When rock weathering takes place by acid rain or plant growth and decay, calcium interacts with water and is transported to another location Water helps calcium move from the land to the oceans High concentrations of dissolved calcium and/or magnesium in fresh water cause hard water When these minerals are concentrated in water, around 89 to 100 parts per million, they don t react well with soap In fact, mineral rings form in bathtubs, and laundered clothes take on a gray color from undissolved soap scum Undissolved minerals in hard water are also deposited in plumbing, coffee pots, and steam irons Frequently, people living in hard water areas use water softeners chemicals that remove calcium and magnesium ions in an exchange with sodium ions Hard water can have benefits In the aquatic environment, calcium and magnesium help keep fish from absorbing metals like lead, arsenic, and cadmium into the bloodstream through their gills Therefore, the harder the water, the less potential for toxic metals to be absorbed by fish In seawater, calcium concentrations are 100 to 1,000 times higher than land levels, and even greater concentrations are found in deeper, colder waters with little circulation Calcium can reside roughly a million years in the ocean before it appears on land again Calcium ions stay in ocean water until they are precipitated out as calcium carbonate Although upper ocean levels are highly saturated with calcium and carbonate ions, saturation depends on location and conditions Photosynthesis and temperature affect warm, shallow water, lowering levels of carbon dioxide These conditions allow calcium carbonate to precipitate either inorganically or through aquatic organisms When calcium carbonate is used by marine inhabitants to build shells, it is called biomineralization As these organisms die, their hard shells sift down to the ocean s floor and gather or dissolve depending on depth, temperature, and pressure Shells sinking to the deepest parts of the ocean often redissolve because of higher carbon dioxide levels in the colder, deeper waters The dividing line separating an area where calcium carbonate dissolves and accumulates is called the lysocline The calcium carbonate deposited by microorganisms is often mixed with other ocean sediments or washed from the land depending on location Birds, animals, and humans eat seafood and shellfish, discarding the shells This returns calcium back to the Earth fairly rapidly However, most calcium is transported by plate tectonics Crustal plates and continental land masses with their mountain-building movement help calcium carbonate deposits move toward the surface in the form of limestone or marble (if changed by pressure and temperature) Figure 103 illustrates the different compounds of the calcium cycle.

The SPUserCodeWebPart has three properties used to locate the wrapped sandboxed Web Part. SolutionId identifies the solution, and TypeFullName and AssemblyName identify the Web Part.

Calcium is taken up by plant roots either directly from the soil or from groundwater When calcium is extracted from the soil via membrane permeability, both active and passive

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15.2.5 Deploying using a site definition If you re building reusable portals and sites, you ve probably been creating, or at least looked at, site definitions. Site definitions are the basis for all sites in SharePoint, and they serve as a template for the sites. They contain, for example, the default activated features and one or more modules that are provisioned when a site is built on a site definition. In SharePoint 2010 the concept of Web Templates are introduced. Web Templates are quite similar to Site Definitions but offer more flexibility and sandbox support. Web Templates should be considered before Site Definitions because they re supported in SharePoint Online, and Site Definitions aren t. The topic of building site definitions could fill a few chapters on its own and there are many opinions on how and when to use them. For our purposes here, it s important to know that you can provision dashboards directly in a site definition using one of the following options:

Deploy the dashboard as a module in the site definition Deploy the dashboard as a feature in the site definition Deploy the dashboard feature to the sites using the site definition with feature stapling Use a provisioning provider as a part of a site definition

transport of ions takes place Calcium is then transferred and stored in the leaves for a time Calcium returns to the soil when leaves fall It is stored in woody plant parts until it decays, is burned, or is consumed by an animal

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