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Vegetation can be lost through a combination of human and natural processes, leading to areas of exposed bare peat frequently accompanied by loss of surface moisture due to drainage or gullying.
As shown in Figure 4, the three samples had a small quantity of weightlessness below 200°C, which was ascribed to the loss of surface moisture and bonded water.
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We also evaluated the impact of surface moisture (soil and vegetation moisture) on the modelling approach.
These layers represent annual mean and variability (standard deviation) of surface moisture.
The function f (moisture) is a function of the surface moisture expressed in terms of moisture content w (kilogram per kilogram) or capillary potential (Pascal) (Cornelis and Gabriels 2003).
Drip loss was calculated by the following equation: Cooking loss was measured at 72 h post mortem as follows: about 20 g of regular-shaped muscle was removed from refrigerator (4°C), and the surface moisture of the fillets was absorbed with filter paper.
Such shading would reduce evaporative loss of soil moisture that had been deposited in the surface layers by hydraulic lift from the taproots, enhancing total water availability and water transport efficiency in this hot, hyper-arid climate.
The weight loss is seen in the three samples during stage I (Table 2) were primarily due to the loss of moisture and were similar to the moisture content values reported in Table 3.
Skin aging is also associated with loss of skin moisture.
Like all humectants, without appropriate occlusion this can actually increase transepidermal water loss by attracting additional moisture from the dermis into the epidermis with ultimate loss of cutaneous moisture into the ambient air.
Thus, the epidermis loses the principle molecule responsible for binding and retaining water molecules, resulting in loss of skin moisture.
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