แปลบทความวิจัยboulders, presence of

แปลบทความวิจัยboulders, presence of crevices, rock pools, depressions, etc. (McCoy
and Bell, 1991), using the chain link method (Beck, 1998). To this
end, we deployed a heavy iron chain and a tape multiple times
across each transect where the quadrat sampling was conducted
(see above). The chain links (length ¼ 2.5 cm) closely followed the
surface and the tape only touched the highest parts of the rocks.
Thus the ratio between the linear distances (tape) vs. the apparent
distance (chain) can be considered as a measure of the structural
complexity of the substratum (hereafter Complexity Index; Beck,
1998). As the AL sampling consisted of contiguous quadrats (see
above) we followed the same protocol for the chain-tape sampling.
We deployed a 1-m long chain and tape (linear distance) multiple
times along a contiguous path, i.e. the beginning of the chain (and
tape) was placed on the end point of the previous chain placement
(15e20 times for each transect), on the breakwater and natural
adjacent platforms along the same transects (totalling 30 to 40
samples for each habitat) where AL sampling was conducted (see
above). In this way, we obtained 30 to 40 measures for the
complexity index for each habitat. At one of the seven study localities
this sampling could only be partially completed (Vi~na del
Mar), given that the strong and persistent wave surge and slope of
the breakwaters at the sampling time (AugusteDecember 2015)
restricted the access to this site. Thus, we only include partial data
sets (10 measures of the Complexity Index) for this locality for
further spatial analyses (see below).
Given inherent differences between intertidal breakwaters (e.g.
made of granite boulders versus cement tetrapods see Fig. 2), we
first conducted a pilot study using three different chain link size;
2.5 cm, 4 cm, and 6 cm per link.We determined that a chain link of
2.5 cmwas sufficient to characterize the spatial distribution of both
granite boulders and tetrapods at the study sites considered, and
consequently all results reported are based on this link size.

ผลลัพธ์ (อังกฤษ) 1:

Translation of articles, research, rock crevices, boulders presence of pools, depressions, etc. (McCoy.and Bell, 1991), using the chain link method (Beck, 1998). To thisend, we deployed a heavy iron chain and a tape multiple timesacross each transect where the quadrat sampling was conducted(see above). The chain links (length ¼ 2.5 cm) closely followed thesurface and the tape only touched the highest parts of the rocks.Thus the ratio between the linear distances (tape) vs. the apparentdistance (chain) can be considered as a measure of the structuralcomplexity of the substratum (hereafter Complexity Index; Beck,1998). As the AL sampling consisted of contiguous quadrats (seeabove) we followed the same protocol for the chain-tape sampling.We deployed a 1-m long chain and tape (linear distance) multipletimes along a contiguous path, i.e. the beginning of the chain (andtape) was placed on the end point of the previous chain placement(15e20 times for each transect), on the breakwater and naturaladjacent platforms along the same transects (totalling 30 to 40samples for each habitat) where AL sampling was conducted (seeabove). In this way, we obtained 30 to 40 measures for thecomplexity index for each habitat. At one of the seven study localitiesthis sampling could only be partially completed (Vi~na delMar), given that the strong and persistent wave surge and slope ofthe breakwaters at the sampling time (AugusteDecember 2015)restricted the access to this site. Thus, we only include partial datasets (10 measures of the Complexity Index) for this locality forfurther spatial analyses (see below).Given inherent differences between intertidal breakwaters (e.g.made of granite boulders versus cement tetrapods see Fig. 2), wefirst conducted a pilot study using three different chain link size;2.5 cm, 4 cm, and 6 cm per link.We determined that a chain link of2.5 cmwas sufficient to characterize the spatial distribution of bothgranite boulders and tetrapods at the study sites considered, andconsequently all results reported are based on this link size.

ผลลัพธ์ (อังกฤษ) 2:

Microsoft Research boulders, crevices of Presence, Rock Pools, depressions, etc. (McCoy
and Bell, 1991st), using the chain link method (Beck, 1 998). To this
End, we deployed a Heavy Iron chain and a Tape multiple times.
Across each transect where the quadrat sampling was conducted
(See above). The chain links (Length ¼ 2.5 cm) closely followed the
surface and the Tape only touched the highest Parts of the Rocks.
Thus the ratio between the linear distances (Tape) VS. . the apparent
Distance (chain) Can be considered as a measure of the structural
complexity of the Substratum (hereafter Complexity Index; Beck,
1998th). As the AL sampling consisted of contiguous quadrats (See
above) we followed the Same Protocol for the chain. -tape sampling.
We deployed a long chain and M-1 Tape (linear Distance) multiple
times along a contiguous path, IE the Beginning of the chain (and
Tape) was Placed on the End Point of the previous chain placement
(for 15e20 times. each transect), on the Breakwater and Natural
adjacent platforms along the Same transects (Totalling 30 to 40
samples for each Habitat) where AL sampling was conducted (See
above). In this Way, we obtained 30 to 40 measures for the
complexity index for. each Habitat. at one of the Seven Study localities
this sampling could only be partially completed (Vi ~ na del
Mar), GIVEN that the strong and Persistent Wave surge and Slope of
the breakwaters at the sampling time (AugusteDecember 2015)
restricted the Access to. this Site. Thus, we only include partial Data
sets (10 measures of the Complexity Index) for this LOCALITY for
further spatial analyzes (See Below).
Given inherent differences between intertidal breakwaters (eg
Made of Granite boulders Versus Cement tetrapods See Fig. 2. ), we
conducted a First Pilot Study using Three different chain link Size;
2.5 cm, 4 cm, 6 cm and per Link.We determined that a chain link of
2.5 Cmwas sufficient to characterize the spatial Distribution of both
Granite boulders and at the tetrapods. Study sites considered, and
consequently all results reported are based on this link Size.

ผลลัพธ์ (อังกฤษ) 3:

Translation research articles, boulders presence of crevices rock pools,,, depressions etc. (McCoy.And, Bell 1991), using the chain link, method (Beck 1998). To this.End we deployed, a heavy iron chain and a tape multiple times.Across each transect where the quadrat sampling was conducted.(see above). The chain links (length ¼ 2.5 cm) closely followed the.Surface and the tape only touched the highest parts of the rocks.Thus the ratio between the linear distances (tape) vs. The apparent.Distance (chain) can be considered as a measure of the structural.Complexity of the substratum (hereafter Complexity, Index; Beck1998). As the AL sampling consisted of contiguous quadrats (see.Above) we followed the same protocol for the chain-tape sampling.We deployed a 1-m long chain and tape (linear distance multiple.)Times along a, contiguous path i.e. The beginning of the chain (and.Tape) was placed on the end point of the previous chain placement.(15e20 times for each transect), on the breakwater and natural.Adjacent platforms along the same transects (totalling 30 to 40.Samples for each habitat) where AL sampling was conducted (see.Above). In this way we obtained, 30 to 40 measures for the.Complexity index for each habitat. At one of the seven study localities.This sampling could only be partially completed (Vi ~ na del.Mar), given that the strong and persistent wave surge and slope of.The breakwaters at the sampling time (AugusteDecember 2015).Restricted the access to this site. Thus we only, include partial data.Sets (10 measures of the Complexity Index) for this locality for.Further spatial analyses (see below).Given inherent differences between intertidal breakwaters (e.g.Made of granite boulders versus cement tetrapods see Fig. 2), we.First conducted a pilot study using three different chain link size;2.5, CM cm 4, 6 and cm per link.We determined that a chain link of.2.5 cmwas sufficient to characterize the spatial distribution of both.Granite boulders and tetrapods at the study, sites considered and.Consequently all results reported are based on this link size.