澳洲论文代写：香港汀角的发展。汀角是位于船湾北岸及西大美督的乡村地区。它现在是一个生态系统保护项目的一部分(农业、渔业和保护部门，2017年)。这是一个柔软的海岸。软岸的形成是由于弱波的作用，或者当斜坡的角度是这样的，波浪带来的颗粒没有被完全带走。这里遗留下来的粒子的净累积量很高。用于海岸开发的颗粒的种类和大小将取决于海浪的强度。空隙的大小取决于海岸干涸的速率。受保护的沙滩通常会有更细的沙子，并且在发展过程中更稳定，因为细沙比粗沙能容纳更多的水分(Martinez等人，2007年)。接下来澳洲论文代写专家将为同学们讲解下有关香港汀角的发展。
龙乐水是一个典型的硬湖。另一方面，坚硬的海岸是由更软的材料组成的，比如暴露在潮汐中的沉积岩。裸露的基岩受到海浪和开阔的海线的影响。建造了陡峭的斜坡，一些平台非常高或狭窄。
栖息地随地域的不同而不同。裸露的岩石海岸承载着许多关于分区的信息(香港公开大学，2013年)。可以识别出不同的区域，如溅水区、潮间带和潮下带。地带性受到生物和非生物因素的影响(Wong, 2002)。非生物因素有波浪作用、潮汐作用、热作用、应力作用等。一些生物因素是幼虫的定居，捕食和行为移动模式在海岸线上。飞溅区是通常被飞溅和飞溅浸湿的区域，不会在任何时候被涨潮淹没(Acosta et al.， 2007)。潮间带为中边缘带，分为潮间带、潮间带和潮间带。这种划分将取决于这些区域被淹没在水中的时间(Doody, 2012)。除了低潮等时候，低潮区是唯一几乎总是受潮汐影响的区域。
就香港而言，在夏季，可以观察到以下情况:飞溅区温度很高，在飞溅区也可以观察到营养物质。潮间带或滨带存在强波浪冲击，温度略低于溅水区。这里可以观察到不规则的小水池。最低区域的温差要大得多。这个地区溶解氧很高，盐度也很高。
Lung Lok Shui is a typical hard shore. Hard shores on the other hand are made of softer materials such as sedimentary rocks that are exposed to the tides. Exposed bedrock is impacted on by waves and an open sea line. Steep slopes are created and some of the platforms are very high or narrow.
Habitats vary as the zonation varies. An exposed rocky shore carries much information on zonation (The Open University of Hong Kong, 2013). Different zones can be identified such as the splash zone, the intertidal zone, and the sub-tidal zone. Zonation is affected and modified by both abiotic and biotic factors (Wong, 2002). Some of the abiotic factors are tat of wave action, tidal action, heat, stress etc. Some of the biotic factors are larval settlement, predation and behavioral mobility patterns on the shore lines. The splash zone is that zone which is usually wetted with splash and spray and would not be immersed in high tide at any time (Acosta et al., 2007). Intertidal zone is considered as the middle fringe zone and it has higher, middle, and lower intertidal zone. This division will be dependent on the amount of time that these zones are submerged in water (Doody, 2012). The sub-tidal zone is the only zone that is almost always under the influence of the tide except for such times like low tides.
For Hong Kong, during the summer time, the following can be observed. The splash zone has a very high temperature, and nutrients can be observed in the splash zone, too. In the intertidal or the littoral zone, strong wave impacts exists, and temperature is little lower than the splash zoned. Small irregular pools could be observed here. The lowest zone is subject to much higher differences in temperature. Dissolved oxygen is high in this region, and salinity.
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